COVER 7/11/05 4:55 PM Page 1 SP-1288 SP-1288 Research and Scientific Support Department e h t f o s e i t i v i t c a e th d n a t h r c o r p a p e s u Re tific S n e t i n c e S m t r a p De 2004 n o t or p e R – 3 0 20 Contact: ESA Publications Division c/o ESTEC, PO Box 299, 2200 AG Noordwijk, The Netherlands Tel. (31) 71 565 3400 - Fax (31) 71 565 5433 Sec1.qxd 7/11/05 5:09 PM Page 1 SP-1288 June 2005 Report on the activities of the Research and Scientific Support Department 2003 – 2004 Scientific Editor A. Gimenez Sec1.qxd 7/11/05 5:09 PM Page 2 2 ESA SP-1288 ISBN ISSN Scientific Editor Editor Published and distributed by Copyright Price Report on the Activities of the Research and Scientific Support Department from 2003 to 2004 92-9092-963-4 0379-6566 A. Gimenez A. Wilson ESA Publications Division © 2005 European Space Agency €30 Sec1.qxd 7/11/05 5:09 PM Page 3 3 CONTENTS 1. Introduction 5 4. Other Activities 95 1.1 Report Overview 5 4.1 95 1.2 The Role, Structure and Staffing of RSSD and SCI-A 5 Symposia and Workshops organised by RSSD 4.2 ESA Technology Programmes 101 Department Outlook 8 4.3 Coordination and Other Supporting Activities 102 1.3 2. Research Activities 11 2.1 Introduction 13 2.2 High-Energy Astrophysics 14 2.3 Optical/UV Astrophysics 19 2.4 Infrared/Sub-millimetre Astrophysics 22 2.5 Solar Physics 26 2.6 Heliospheric Physics/Space Plasma Studies 31 2.7 Comparative Planetology and Astrobiology 35 2.8 Minor Bodies 39 2.9 Fundamental Physics 43 2.10 Research Activities in SCI-A 45 3. Scientific Support Activities 53 3.1 Astrophysics Missions Division 56 3.2 Solar and Solar-Terrestrial Missions Division 64 3.3 Planetary Missions Division 70 3.4 Fundamental Physics Missions Division 78 3.5 Space Telescope Operations Division 80 3.6 Science Operations and Data Systems Division 83 3.7 Science Payload and Advanced Concepts Office 89 Annex 1: Manpower Deployment 107 Annex 2: Publications (separated into refereed and non-refereed literature) 113 Annex 3: Seminars and Colloquia 149 Annex 4: Acronyms 153 Sec1.qxd 7/11/05 5:09 PM Page 5 introduction 5 1. INTRODUCTION 1.1 Report Overview This report on the activities of the Research and Scientific Support Department (RSSD) covers the 2-year period of 2003-2004. It is prepared as input to the Department’s Advisory Committee, a group of independent external scientists invited by the Director of ESA’s Scientific Programme to review the Department’s activities. It forms the basis of the oral reports made to ESA’s Space Science Advisory Committee and the Science Programme Committee every second year. Through the publication of the report as an ‘SP’ (Special Publication) by the ESA Publications Division, the activities of the Department are brought to the attention of the scientific community and to a broader audience. These Biennial Reports have been produced since 1980. In this volume, a number of changes introduced in the last report have been kept. The report also covers the activities of the Science Payload and Advanced Concepts Office (SCI-A) owing to its close links with many activities in RSSD and its history as the previous Science Payload Technology Division. The report is divided into four Chapters plus four Annexes. Chapter 1 deals with the Department’s role and organisation. A brief summary is given because its mandate and structure did not change significantly during the reporting period. Reference should be made to the previous report (ESA SP-1268) for further information. The names of staff, their locations, their functional duties and scientific research interests are given in Annex 1. Chapter 2 addresses the scientific research of the Department’s staff, broken down according to ‘discipline’ rather than divisional structure. A complete listing of the scientific papers published in the literature is given in Annex 2. Some 340 refereed papers were published during 2003 and 2004, and more than 350 conference papers and other publications appeared. Chapter 3 provides a top-level summary of the missionrelated activities at Divisional level. For the four Missions Divisions, the prime contributions to the scientific support of the various elements of the Science Programme are summarised. For the two Operations Support Divisions, special mention is also made of postoperational and archiving phases. The activities of SCI-A are included. Finally, Chapter 4 addresses a variety of activities carried out by RSSD in its support role to the community. The Chapter summarises important scientific symposia and workshops organised by the Department, support to the Directorate’s science communication activities, and various other activities. While this Biennial Report provides perspective on the breadth and quality of the activities of the staff, both in their research and functional work, it is not intended to be comprehensive. Up-to-date information on the Department’s activities can be obtained at http://www.rssd. esa.int and for SCI-A at http://sci.esa.int/science-e/ www/area/index.cfm?fareaid=65 1.2 The Role, Structure and Staffing of RSSD and SCI-A RSSD, one of the two Departments of ESA’s Scientific Directorate, provides the direct interface to the scientific community throughout all mission phases. Following in-orbit checkout and commissioning, it is also responsible for the management of the missions. In addition, the Department plays its part in the dissemination of scientific knowledge to the public and for educational purposes. In essence, the role of RSSD is to ensure the best possible scientific performance of ESA’s Scientific Programme missions. To this end, the Department is responsible for the implementation of all science management aspects of the missions in the Science Directorate throughout their study and operations phases. In particular, the Department is responsible for providing scientific expertise to studies and projects in all phases, and for ensuring that maximum scientific return within practical technical and budgetary constraints is maintained as a target through all phases of a scientific mission. The Department also manages, through its study or project scientists, the activities of each mission science team. RSSD is responsible for all aspects of science operations (definition, development, implementation and execution) through all phases of missions and manages the operations phases of missions following in-orbit commissioning, supported, as necessary, by system engineering expertise from the Scientific Projects Department. In very close coordination with SCI-A, RSSD provides scientific and payload expertise within the Agency in all phases of scientific missions, including to other directorates of the Agency (e.g. on International Space Station payloads). It works with external science teams to define the science requirements for future mission Sec1.qxd 7/11/05 5:09 PM Page 6 6 introduction Head of Research and Scientific Support Department SCI-S Chief Scientist SCI-SR Astrophysics Missions Division SCI-SA Science Operations and Data Systems Division SCI-SD Planetary Missions Division SCI-SB Space Telescope Operations Division SCI-SN Solar & Solar-Terrestrial Missions Division SCI-SH Fundamental Physics Missions Division SCI-SP Figure 1.2/1: The structure of RSSD. studies and associated payloads and passes these to SCI-A for follow-up. It is, of course, very important that the scientific staff of both RSSD and SCI-A maintain their scientific proficiency by undertaking personal research. In order to discharge its responsibilities and tasks in an efficient manner, the Department is structured into four Missions Divisions: — — — — the Astrophysics Missions Division; the Planetary Missions Division; the Solar and Solar-Terrestrial Missions Division; the Fundamental Physics Missions Division; and two Operations Support Divisions: — the Science Operations and Data Systems Division; — the Space Telescope Operations Division. The Office for Science Payload and Advanced Concepts (SCI-A) is under the direct authority of the Director of the Scientific Programme. This Office is responsible for the assessment phase and the strategic approach for Figure 1.2/2: The structure of SCI-A. future missions as well for new payload technologies in support of the Cosmic Vision long-term Scientific Programme. The Office works, in close liaison with the RSSD study scientists and the science community, to determine the science and technological needs of this programme. In addition, SCI-A provides payload support/expertise to missions under development, both to RSSD Project Scientists as well as the Science Projects Department. The Office is also responsible for laboratory support throughout the Directorate, including those RSSD research activities requiring such support. The organigram of RSSD is shown in Fig. 1.2/1. In addition, the office of the Department Head is supported by a budget control group including three integrated project controllers from SCI-M. The role and functions of the six Divisions, and those of SCI-A, are described further in Chapter 3. The staff of the Department (37 at the end of 2004) and of SCI-A (21, including 2 advanced recruitments) hold posts within the overall ESA staff complement. Staff associated with Science Operations Teams are generally supernumerary positions. By the end of 2004, there was a complement of 68 supernumeraries (3 in SCI-A). Fig. 1.2/2 depicts the structure of SCI-A. It should be noted that, in these teams, many contractors and often staff from Principal Investigator (PI) institutes work together in an integrated structure. An overview of the staff in post at the end of 2004 is given in Table 1, integrating personnel from RSSD proper and SCI-A. Figure 1.2/3 gives the distribution of staff according to functions within RSSD. Department staff are located not only at ESTEC, close to the Science Directorate’s project teams and the Technical Directorate, but also in Villafranca (ISO and XXMNewton science operations teams), in Garching and Baltimore (Space Telescope Operations Division) and Greenbelt (SOHO Project Scientist Team at NASA Goddard Space Flight Center). During 2004, the Villafranca facilities were integrated into the European Space Astronomy Centre (ESAC). Figure 1.2/4 shows the distribution according to location of personnel from RSSD. While not formally on the ESA staff complement, Internal Research Fellows, on contracts of maximum Sec1.qxd 7/11/05 5:09 PM Page 7 introduction 7 Table 1: RSSD Staff in Post at end of 2004. Head of Department: A. Gimenez Assistant Administrator: C. Bingham Divisional Assistants: S. Ihaddadene, B. Schroeder, C. Villien Chief Scientist: B.H. Foing Astrophysics Missions Division J. Clavel (Head) M. Fridlund T. Boeker A. Heras J. de Bruin P. Jakobsen F. Favata R. Laureijs S. Leeks A. Marston Project Controller: R. Fontaine* R. Davis* G. D’Aquino* *seconded from SCI-M A. Parmar M.A.C. Perryman G.L. Pilbratt T. Prusti J. Tauber R. Vavrek H. Laakso R.G. Marsden L. Sanchez Duarte* T.R. Sanderson R.M. Schulz L.H. Svedhem K. Wirth O. Witasse A. Clampin-Nota H. Jenkner I. Kamp J. Maiz-Apellaniz M. Miebach B. Mobasher N. Panagia M. Robberto M. Sirianni E. Villaver T. Wiklind M.J. Szumlas D. Texier** G. Thoerner A. Toni C. Winkler J.J. Zender Integral Science Operations L. Hansson (Head) P. Barr L. O’Rourke A. Orr J. Sternberg ISO Data Centre (ESAC) A. Salama (Head) R. Lorente E. Verdugo M. Arpizou M. Ehle J.C. Gabriel M. Guainazzi J. Hoar M. Kirsch Solar and Solar-Terrestrial Missions Division H. Opgenoorth (Head) C.P. Escoubet B.G. Fleck* S. Haugan* *located at SOHO/EOF, NASA Goddard Space Flight Center Planetary Missions Division G. Schwehm (Head) A. Chicarro D.V. Koschny J.-P. Lebreton P. Martin Fundamental Physics Missions Division R. Reinhard (Head) L. Cacciapuoti O. Jennrich Space Telescope Operations Division D. Machetto (Head) M.R. Rosa D. Sforna ST-ECF (Garching) STScI (Baltimore) R. Albrecht R.A.E. Fosbury A. Aloisi A. Micol S. Arribas Science Operations and Data Systems Division M.F. Kessler (Head) F. Jansen C. Arviset* N. Schartel* K. Bennett *located at ESAC **located at Geneva P. Garcia Lario XMM-Newton Science Operations (ESAC) L. Metcalfe (Head, Science Support) J. Munoz Peira (Head, Instrument Operations) B. Altieri A. Pollock M. Santos-Lleo Herschel Science Operations Development J. Riedinger S. Ott Science Payload and Advanced Concepts Office (Science Payloads Technology Division) A. Peacock (Head) T. Beaufort P. Falkner D. Klinge S. Andersson J.F. van der Biezen Ph. Gondoin D. Lumb T. Appourchaux B.A.C. Butler J. Heida D. Martin H.J. Arends A. van Dordrecht B. Johlander N. Rando M. Bavdaz C. Erd J. Romstedt L.C. Smit U. Telljohann J. Verveer Sec1.qxd 7/11/05 5:09 PM Page 8 8 introduction Figure 1.2/3: Distribution of RSSD staff according to prime function. Figure 1.2/4: Distribution of RSSD staff according to location. 2 years and funded by the Agency’s Education budget, play a major role in the Department’s research activities. Typically, some 15 Research Fellows were in post at any one time during the reporting period. The Department and SCI-A also hosted several Young Graduate Trainees on 1-year contracts, and offered numerous opportunities for trainees and stagiaires. 1.3 Department Outlook Highlights for the Department in the reporting period include: — the successful launches of Mars Express, SMART-1, Rosetta and Double Star, and the very promising first data from all their instruments; — the successful arrival of Cassini-Huygens at Saturn and the release of the Huygens probe towards Titan; — the excellent scientific results from Mars Express during its first year in orbit around the Red Planet; — RSSD and SCI-A contributions to the planning of ESA’s long-term Scientific Programme ‘Cosmic Vision’, covering the decade 2015-2025; — the completion, testing and delivery of Co-Investigator contributions to Rosetta and SMART-1 instruments; — the continued excellent science return from the HST, Ulysses, SOHO, Cluster and XMM-Newton missions in orbit; — maintaining a high level of research with a significant number of publications in spite of the increasing pressure of the scientific support activities; — the active organisation of a number of symposia and workshops for the space science community; — transfer of the BepiColombo mission to Mercury from the assessment phase to implementation phase. In 2004, RSSD achieved an all-time record of missions in orbit under its responsibility. A total of 11 space missions (comprising 14 spacecraft) were being operated, with an impact on the Department’s efforts in the area of science operations despite the frozen level of complement. During the past 2-years, time was devoted to consolidating the reorganisation of the Department in line with its new role and goals. In addition, some refinements in the internal working procedures of the Directorate were found necessary. The next 2 years are expected to see a review of the effectiveness of the structure in place and the performance of the staff at all levels, with the possibility of more changes if required for the achievement of the overall goals of the Department. Moreover, further discussions are expected within the Directorate to improve interfaces with the Projects Department and other Offices, and new areas of cooperation with other Directorates, such as the newly created programme for Exploration, will need to be expanded. At the level of the Scientific Programme, the challenges of the coming years are clearly dominated by the definition of the new Cosmic Vision plan for the decade 2015 to 2025. Many discussions and evaluations will have to be done in close cooperation with the scientific community and our Advisory Bodies to define the themes, and then the missions to be implemented, to achieve the selected scientific goals. While the last 2 years were devoted to implementing a previously approved programme under increasingly difficult budgetary circumstances, we can now look into the future for new targets and science. Of course, we are still not clear of the problems with the current programme, but we certainly have to start the discussion on what missions should be launched in little more than 10 years from now, in order to keep a stable European contribution to space science. The way to define and implement missions is also changing considerably. For example, the use of themes, rather than the usual call for ideas, is allowing us to study new technologies not constrained by existing studies or projects and to look for the actual scientific needs in the Sec1.qxd 7/11/05 5:09 PM Page 9 introduction reference decade instead of trying to just do ‘more of the same’. In particular, SCI-A is responsible for the assessment of all future missions within the Directorate and is therefore closely linked to RSSD and the technology development activities. In the implementation of missions, lessons learnt have been introduced together with a more systematic risk analysis for each mission. In particular, for the Department’s domain, the design and implementation of science operations has become more pro-active and new ideas will have to be implemented in the next years to ensure a more efficient performance of the operation of planetary missions. Concerning the research activities in the Department, the coming years will focus on the increasing recognition, and evaluation, of the results achieved by the staff. Another point of importance is the rapidly increasing need to devote time to functional activities to the detriment of the time available for research – a dangerous situation that should be avoided. Nevertheless, research cannot be dictated and an average allocation of 20% of the time may not be enough for competitive science. It is important to see how these activities develop and whether further adjustments will be necessary in the light of experience. Our opportunities for the analysis of data provided by missions in orbit are now enhanced by those offered by SMART-1, Mars Express, the arrival of Cassini at Saturn and the very recent entry of the Huygens probe into the atmosphere of Titan. In astronomy, the data exploitation of successful missions such as Integral, XMM-Newton and HST or ground-based observatories continues, as well as that of data archives from previous missions like ISO that are currently being enhanced through the development of virtual observatories. In the area of the Solar System, research flourishes, in close collaboration with partners in the scientific community, thanks to Ulysses, SOHO and Cluster data. New flight instrumentation is under development through contributions to the COROT and STEREO missions. Finally, we have seen in the past 2 years the beginning of an effort in the area of Fundamental Physics research that should develop further. Scientific support activities to missions under development or study will require close attention. Continued efforts will be devoted to the preparation of Herschel and Planck, which are entering critical phases of their development, as well as to the European contribution to JWST. On the other hand, Gaia will begin its implementation phase and the preparation of the very demanding science operations will require special attention. The gravitational wave observatory LISA and its technology mission LISA Pathfinder will require special efforts in this emerging area of space science. In the Solar System domain, our activities will focus on Venus Express, to be launched in 2005. Equally, the preparations for BepiColombo, travelling to Mercury, and of Solar Orbiter will need to be intensified. 9 One of the important responsibilities of RSSD – the science operations of the various scientific missions – continues to require our full attention as well as the further development of skills and tools to cope with an increasingly demanding activity. The availability of properly processed scientific data, to the full satisfaction of the scientific community at large and valid for both observatory-type missions, with its high pressure from the scientific community, and PI-type missions, is a clear objective. For SCI-A, one of the key tasks is the technical assessment of all future missions within the Directorate coupled to long-term planning, both at mission level and for technology development. Such technology planning is assisted by a parallel Technology Research and Development Programme. To conclude, while the need to maintain and, where necessary, to improve the links with the research institutions in Member States through active cooperative programmes remains a prime goal of the Department, other aims for the future include the continued provision of properly processed scientific data to the community and support to the development of science communications and science education activities in ESA. sec2.qxd 7/11/05 5:12 PM Page 11 11 2. RESEARCH ACTIVITIES IN RSSD AND SCI-A 2.1 Introduction 2.2 High-Energy Astrophysics 2.2.1 2.2.2 2.2.3 2.2.4 Stellar coronae and star-formation regions X-ray binaries Galaxies and active galactic nuclei Ground-based photon-counting studies 2.3 Optical/UV Astrophysics 2.3.1 2.3.2 2.3.3 2.3.4 2.3.5 The Helix Nebula: when opportunity knocks Central stars of planetary nebulae Identifying core-collapse SN progenitors Metals in the dwarf starburst galaxy NGC 1705 Luminous IR galaxies: a key galaxy population 2.4 Infrared/Sub-millimetre Astrophysics 2.4.1 2.4.2 2.4.3 2.4.4 2.4.5 Solar System studies Interstellar medium studies Star formation Stellar studies Extragalactic studies 2.5 Solar Physics 2.5.1 2.5.2 2.5.3 2.5.4 Chromospheric oscillations Dynamics of transition region blinkers Comparison of blinkers and explosive events Coronal magnetic fields 2.6 Heliospheric Physics/Space Plasma Studies 2.6.1 Energetic particles from the October/November 2003 solar events Energetic particles in the high-latitude, highspeed solar wind Acceleration of electrons in the auroral region Magnetospheric observations Examples of other associated activities within SCI-SH 2.6.2 2.6.3 2.6.4 2.6.5 2.7 Comparative Planetology and Astrobiology 2.7.1 2.7.2 2.7.3 2.7.4 2.7.5 2.7.6 Mars research Lunar studies Cassini-Huygens data analysis preparation Ground-based observations of Titan winds Earth comparative planetology Astrobiology 2.8 Minor Bodies 2.8.1 2.8.2 2.8.3 2.8.4 2.8.5 The MIDAS instrument on the Rosetta mission Determination of isotopic ratios in comets Characterisation of the new Rosetta target comet Comet modelling Ground-based observations of comets 2.9 Fundamental Physics 2.9.1 2.9.2 2.9.3 Interferometer design for LISA Pathfinder A phasemeter for LISA Pathfinder Frequency stabilisation for LISA 2.10 Research Activities in SCI-A 2.10.1 2.10.2 2.10.3 2.10.4 Development of superconducting cameras Advanced semiconductor sensors Development of advanced optics Advanced instrumentation research for planetary missions sec2.qxd 7/11/05 5:12 PM Page 13 research activities 13 2.1 Introduction contracts, as well as Portuguese and Spanish Trainees on 2-year grants funded by their respective nations. The Department also hosted a number of Stagiaires for durations of up to 6 months, as part of their research or graduate engineering studies, as well as externally supported research students. The scheme for Internal Research Fellows, Trainees and Stagiaires, besides offering training and experience at RSSD, permits a continuous exchange and collaboration with their institutes of origin or with their future destinations. A number of Master or PhD theses were co-supervised by RSSD and SCI-A staff scientists and colleagues from academic institutes. Research in RSSD and SCI-A is an integral part of the activities of the scientific staff, needed to maintain and develop its scientific skills, peer recognition and handson experience in space science. Active involvement in research is necessary for Staff Scientists to remain part of the community when performing their mission-related duties. The overall research programme is organised in thematic research groups covering different areas in astrophysics (high-energy, optical/UV, IR/sub-mm); solar physics, heliospheric and space plasma physics; comparative planetology and astrobiology; minor bodies; fundamental physics; development and exploitation of superconducting cameras for astronomy. These topics reflect the breadth of the Cosmic Vision programme within the different fields related to ESA science missions. The results of these research activities, as well as new proposals for the following year, are reviewed annually, and the overall RSSD research programme is assessed by an external visiting committee every 2 years. The activities have been influenced by the opportunities given by the ESA Science Programme, but are constrained by the limited time available to scientists owing to increased workload on projects, studies and other functional activities. In addition, in support of future missions and long-term planning, SCI-A conducts an independent laboratory-based Technology Research and Development Programme in close coordination with other Programmes of the Agency. RSSD and SCI-A staff undertake research collaborations with external institutes from all the Member States and with the international community, both in instrument development and data exploitation for ESA and international space science missions. External researchers have also contributed to the scientific output of the department in the form of extended visits to RSSD and SCI-A. The Research Groups provide a basis for the integration and daily research activities of Research Fellows and Trainees, with the Chief Scientist responsible for their overall supervision. ESA Internal Research Fellows, on post-doctoral contracts of up to 2 years, play a major role in the Department’s research activities. On average, some 15 internal Research Fellows are in post at any one time, covering the large range of topics in RSSD. They are recruited through the standard ESA process of interviews. The excellence and publication record of candidates, their research programme matching RSSD research priorities, and the training opportunities at RSSD for their future career prospects are prime selection criteria. RSSD is also hosting a Post-Doctoral Researcher funded through the EU European Network collaboration scheme. The Department, together with SCI-A, hosts Young Graduate Trainees on 1-year Mention should also be made of the role of 20 ESA external post-doctoral Research Fellows, funded to work 1 or 2 years in ESA Member States’ institutions. They contribute in the building of research networking in support of ESA missions. There are two calls per year (applications due end of March and end of September) covering all aspects of post-doctoral research related to ESA activities in space science as well as Earth observation, microgravity and human spaceflight and space technologies. RSSD and SCI-A scientists publish, on average, some 180 refereed papers per year (those published or accepted in 2003 and 2004 are listed in Annex 2). They still manage to maintain a leading role in more than a third of their research papers, despite the functional workload in scientific support to projects, thanks to their commitment, collaborations within research groups and with the outside community, and the contributions by Research Fellows. RSSD staff organised Workshops or Symposia in support of ESA science missions or in relation to scientific themes or collaborative research topics (Section 4.1). They also contributed to several coordination and supporting tasks (Section 4.3), as well as science communications and education activities (Section 4.4). A programme of seminars for the Department (also open to other interested scientists) invites external scientists to present results or reviews over a wide range of space science topics (Annex 3). The successful colloquia programme presenting prestigious speakers to all ESTEC staff continued during the reporting period (Annex 3). Also, within a programme of internal seminars, RSSD scientists report on their ongoing research activities or give tutorials for their colleagues across disciplines. The following Sections are arranged according to the individual research lines. sec2.qxd 7/11/05 5:12 PM Page 14 14 research activities 2.2 High-Energy Astrophysics The High-Energy Astrophysics research group uses primarily XMM-Newton observations coupled with extensive ground-based facilities to address a wide range of issues. Topics such as stellar physics and accretiondriven objects are the focus of the group’s attention. 2.2.1 Stellar coronae and star-formation regions Using XMM-Newton data, Favata et al. (2004) reported the first clear evidence for an X-ray cycle in a star other than the Sun. During the 11-year solar cycle, the X-ray luminosity of the Sun varies in the 0.7-2.5 keV band by some 2 orders of magnitude, yet the X-ray luminosity of most active stars (which have X-ray luminosity 100-1000 times greater than the Sun) is remarkably constant, within a factor of 2 or so, across several years. A dedicated programme has been set up to monitor, at 6-month intervals, the X-ray luminosity of the solar analogue HD 81809, which has an X-ray activity level comparable to the Sun (thus much lower than the typical targets of X-ray spectroscopic observations). The results of the first 3 years of the programme are given in Fig. 2.2.1/1; they show that the X-ray luminosity of HD 81809 has varied by more than one order of magnitude in the last 2 years, and, according to the phase of the known chromospheric cycle observed in the Ca II H&K lines, is expected to bottom out between 2005 and 2006. The XMM-Newton observing programme Figure 2.2.1/1: Three years of XMM-Newton observations of HD 81890 (square symbols), together with the Mt. Wilson observations of the Ca II chromospheric activity index of the same star (crosses). The very large long-term variation in X-ray luminosity, with a maximum in mid-2002, is easily seen. (From Favata et al., 2004). Figure 2.2.1/2: The coronal abundances of λ And, plotted with its measured photospheric abundances. Note how both differ in a similar way from the solar photospheric composition (from Sanz-Forcada et al., 2004). continues throughout 2005 and will be re-proposed for each future AO, aiming to observe at least one complete cycle (HD 81809 has a chromospheric cycle duration of 8.2 years). Chemical abundances of the coronal plasma in active stars are an ongoing subject of debate. The discovery from early ASCA spectra that the coronal plasma does not have the composition of the solar photosphere (with generally lower abundances reported) sparked a long discussion about the actual abundance patterns and the possible fractionation mechanisms. Progress has, however, been hampered by the lack of photospheric abundances for most active stars – the only stars sufficiently X-ray bright for their high-resolution X-ray spectrum to be observed and coronal abundances derived. A long-term programme to determine both the photospheric and coronal chemical abundances of individual active stars is being carried out in RSSD in collaboration with a number of institutions. The most recent results (Fig. 2.2.1/2) come from the analysis of XMM-Newton and Chandra high-resolution spectra of a number of active stars (Sanz-Forcada et al., 2004). This has shown that, in a number of specific cases, the coronal abundances, which would be very different to solar photospheric abundances, are actually very similar to their stellar photospheric abundances. However, these RS CVn-type active binary stars have themselves rather strange photospheric abundances (Morel et al., 2004). The structures of the coronae in active stars and their comparison with the solar corona, the only spatially resolved corona we can observe, have been open questions since the beginning of imaging X-ray astronomy. The advances in both collecting area and sec2.qxd 7/11/05 5:12 PM Page 15 research activities spectral resolution brought by XMM-Newton and Chandra have allowed new statistics to be exploited, namely the rotational modulation of spectral Doppler shifts and of the global X-ray luminosity. Hussain et al. (2005) studied the prototypical young main sequence star AB Dor with a long Chandra LETG observation, and found significant modulation in both the Doppler velocity of the O VIII coronal line (with an amplitude of about 60 km/s) and in the X-ray luminosity (at the 1015% level). This implies a highly non-homogeneous corona, with the X-ray emission dominated by a small number of compact emitting regions located at high latitudes. These observations also rule out a corona composed of very big magnetic loops (significantly larger than the star itself), which were in the past thought to be present on very active stars. The origin of the observed strong X-ray activity in intermediate mass young stars (Herbig Ae/Be stars, HAeBe in short) remains a puzzle: these stars are not expected to have a convective zone sustaining a dynamo, and their winds are thought not to be energetic enough to generate the observed X-rays through a wind shock mechanism (thought to be the origin of the X-ray emission observed in the more massive O and early B stars). In a number of cases, low-mass companions have been discovered to be the origin of the observed X-rays; however, there remains a significant number of apparently single HAeBe stars. Combining XMMNewton and Chandra data, Giardino et al. (2004) have for the first time detected flaring activity from an apparently single HAeBe star, V892 Tau. The characteristics of the flares, one of which has a peak temperature of around 90MK, require the plasma to be magnetically confined, ruling out classical wind shock models (in which the plasma is essentially unconfined). While the origin of the magnetic field is still unclear, detailed analysis of the flares constrain the magnetic field at around 500 G. 15 Figure 2.2.2/1: XMM-Newton EPIC pn residuals when the best-fit model is fitted to XB 1254-690 spectra for observations when a deep dip is present (2001 Jan) and no dipping is evident (2002 Feb). The absence of any overall change in absorption line properties indicates that their presence is not related to the presence, or absence, of dips. from MXB 1659-298, GX 13+1 and 4U 1624-49. In the last 2 years, these results have been extended by observations of two more dip sources, XB 1254-690 (Boirin & Parmar, 2003) and XB 1916-053 (Boirin et al., 2004). Ongoing analysis of all the dip sources observed by XMM-Newton is allowing their global properties to be investigated. 2.2.2 X-ray binaries During Exosat observations, the LMXB XB 1254-690 exhibited irregular dips in X-ray intensity that repeated every 3.88 h. The dips are almost certainly due to obscuration in the thickened outer regions of an azimuthally structured accretion disc. One of the peculiarities of this source is that, during some observations, deep (up to 80%) dipping is present but in others it is completely absent, while the overall X-ray intensity is unchanged. During an XMM-Newton observation in January 2001 a deep X-ray dip was seen while, true to form, in a second observation a year later no dips were evident. The 0.5-10 keV EPIC spectra from both non-dipping intervals were very similar, being modelled by a disc-blackbody and a power-law continuum with additional structure around 1 keV and narrow absorption features at 7.0 keV and 8.2 keV that are identified with the K-alpha and K-beta absorption lines from H-like Fe. The low-energy structure may be modelled as a 175 eVwide emission line. The absorption line properties show no obvious dependence on orbital phase and are similar in the two observations (Fig. 2.2.2/1), suggesting for the first time that the occurrence of such features is not directly related to the presence of dipping activity. The outstanding spectral resolution and sensitivity of XMM-Newton continues to be exploited to investigate narrow absorption features in low-mass X-ray binaries (LMXBs). In the previous report, results were reported The discovery of narrow Mg XII, Fe XXV and Fe XXVI K-alpha X-ray absorption lines in the persistent emission of the dipping LMXB XB 1916-053 during an XMMNewton observation in September 2002 has been References Favata, F., Micela, G., Baliunas, S.L. & Schmitt, J.H.M.M., 2004, A&A 418, L13. Giardino, G., Favata, F., Micela, G. & Reale, F., 2004, A&A 413, 669-679. Hussain, G.A.J., Brickhouse, N.S., Dupree, A.K. et al., 2005, ApJ 621, 999. Morel, Th., Micela, G., Favata, F., Katz, D. & Pillitteri, I., 2004, A&A 412, 495. Sanz-Forcada, J., Favata, F. & Micela, G., 2004, A&A 416, 281. sec2.qxd 7/11/05 5:12 PM Page 16 16 research activities consistent with a decrease in the amount of ionisation, as dipping activity progresses. This implies the presence of cooler material in the line of sight during dipping, consistent with the decrease in energy of the Fe feature as dipping becomes more intense (Fig. 2.2.2/2). The discovery of a 0.98 keV absorption edge in the persistent emission spectrum is also reported. The edge energy decreases to 0.87 keV during deep dipping intervals. The detected feature may result from edges of moderately ionised Ne and/or Fe, with the average ionisation level decreasing from persistent emission to deep dipping. This is again consistent with the presence of cooler material in the line of sight during dipping. References Boirin, L. & Parmar, A.N., 2003, A&A, 407, 1079. Boirin, L., Parmar, A.N., Barret, D., et al., 2004, A&A 418, 1061. 2.2.3 Galaxies and active galactic nuclei The X-ray emission from advection-dominated accretion flows in the elliptical galaxy NGC 3226 has been studied (Gondoin et al., 2004)). The continuum can be described by a bremsstrahlung model absorbed by neutral material. The absence of variability suggests that the emission originates from regions relatively far from the nucleus. Based on luminosity considerations, the mass of the central accreting black hole is be constrained to be 1.750x107 solar masses. Figure 2.2.2/2: The variation in the Fe absorption feature seen from XB 1916-053 during dipping intervals. The energy of the feature is indicated by vertical tick marks. The mean energy of the feature decreases with increasing dip depth, consistent with the presence of increasingly cooler material. reported (Boirin et al., 2004). Such absorption lines from highly ionised ions are now observed in a number of high-inclination (close to edge-on) LMXBs, such as XB 1916-053, where the inclination ranges between 60° and 80°. This, together with the lack of any orbital phase dependence of the features (except during dips), suggests that the highly ionised plasma responsible for the absorption lines is located in a cylindrical geometry around the accretion disc. Using the ratio of Fe XXV and Fe XXVI column densities, the photo-ionisation parameter was estimated to be 103.92 erg cm/s. Only the Fe XXV line is observed during dipping intervals and the upper-limits to the Fe XXVI column densities are The first systematic investigation of magnetic fields in barred spiral galaxies is now complete (Harnett et al., 2004; Beck et al., 2002). The radio surface brightness is found to be highest in galaxies with a long bar. The derived regular magnetic fields are significantly different from those in non-barred galaxies, allowing new constraints to be placed on dynamo-models. Individual follow-up studies (including a comparison with X-ray observations) are continuing. XMM-Newton observations of nearby star-burst galaxies have been analysed as part of a multi-wavelength investigation of all phases of the extra-planar interstellar medium (Ehle et al., 2004; Dahlem et al., 2003). This study was conducted in order to assess the importance of haloes as repositories of a metal-enriched medium and their significance in terms of galactic chemical evolution. The common goal of the multi-wavelength (X-ray, radio continuum, H I and optical) project is to obtain a better understanding of star-formation related outflows. The galaxy NGC 4666 (Fig. 2.2.3/1) is an example of the observed interplay between X-ray and optical filaments, star-formation regions in the underlying disc, and the magnetic field structure. Analysis of XMM-Newton’s observation of the Seyfert 1 galaxy ESO 141-G55 has revealed, in addition to an Fe sec2.qxd 7/11/05 5:12 PM Page 17 research activities 17 Newton observation of Mkn 304 (Piconcelli et al., 2004), it seems likely that such absorbers are characteristic of X-ray weak quasars in general. They are different from the warm absorbers found commonly in AGNs that show much lower column densities and ionisation parameters. The X-ray spectrum of PG 1535+547 shows a relativistic Fe K-alpha disc line from fluorescence emission and is therefore only the second X-ray weak quasar with such an unusual characteristic. The occurrence of a variable relativistic Fe K-alpha fluorescence line in two out of the five well-studied X-ray weak quasars may indicate that such features are more common in these systems. Figure 2.2.3/1: A pn-MOS 0.5-0.9 keV image of NGC 4666 overlaid on an H-alpha and N II optical narrowband image. In the halo, the most extended optical emission line filaments, which form an X-shaped structure, reach out to distances above the plane by up to ~7.5 kpc. Vectors mark the orientation of the magnetic field observed at 4.89 GHz with the VLA; their lengths are proportional to the polarised intensity. K-alpha fluorescence line (equivalent width of ~40 eV), an absorption edge at 7.6±0.1 keV (Gondoin et al., 2003a). Similar results have been obtained for the Seyfert 1 galaxy NGC 3227 by Gondoin et al. (2003b). At soft energies, the spectrum of NGC 3227 shows strong continuum absorption of 6.5x1022/cm2. XMM-Newton spectra of 40 quasars with redshifts < 1.72 from the Palomar-Green Bright Quasar Survey sample have been analysed (Piconcelli et al., 2005; Jimenez-Bailon et al., 2004). The hard X-ray continuum emission > 2 keV can be modelled by a power-law with mean 2-12 keV photon index of 1.89±0.11. Below 2 keV, a strong broad excess is present in most spectra, for which it is impossible to find an universal spectral shape. Warm absorber features are present in around half of the sources, in contrast to their rare occurrence (~5-10%) in previous studies. The XMM-Newton view of opticallyselected bright quasars therefore suggests that there is no significant difference in their X-ray spectral properties when compared with low-luminosity Seyfert 1 galaxies. Three X-ray weak quasars observed with XMM-Newton have been studied (Schartel et al., 2004). All three objects are absorbed by ionised material with high column densities and ionisation parameters. In combination with the similar result from the XMM- The discovery of two new occurrences of extreme variations in the column density obscuring nearby AGN has been reported (Guainazzi et al., 2004). The typical timescale of these phenomena is ~50 yr. This provides further support to a scenario in which gas associated with the host galaxy, or with dense regions of enhanced star formation, is responsible for obscuration in 50% of the AGN in the nearby Universe, which is inconsistent with the predictions of the standard AGN Unification model. The ongoing investigation of the star-formation processes in the nuclei of spiral galaxies has been expanded. Following up on the previous Hubble Space Telescope survey of nuclear star clusters, Boeker and collaborators (Boeker et al., 2002) have used an isophotal analysis to demonstrate that many late-type spirals are indeed ‘pure’ disc galaxies in that they show no evidence for a spheroidal bulge component. The team has then used the IRAM 30 m telescope to search for molecular gas in the central kpc of 47 bulge-less spirals in order to measure the fuel reservoir available for nuclear star formation. The results demonstrate that a large fraction of galaxies contain enough gas in the vicinity of the nucleus to sustain at least a few modest (about 105 solar masses in new stars) star-burst episodes. This is consistent with scenarios that invoke nuclear cluster growth through repetitive star-bursts. The challenge then is to explain how the gas can lose its angular momentum and be funnelled to within a few pc of the galaxy nucleus. In order to advance observations at this level of detail, Boeker and collaborators have performed a detailed case study of IC342, a nearby, late-type spiral with a prominent nuclear star cluster. Their observations with the Owens Valley Radio Interferometer revealed a molecular disc that coincides with the nuclear star cluster and has a radius of only 15 pc. This demonstrates that molecular gas can indeed accumulate on such scales, making repetitive nuclear star-bursts a plausible scenario. References Beck, R., Shoutenkov, V., Ehle, M. et al., 2002, A&A 391, 83. Boeker, T., Laine, S., van der Marel. R. et al., 2002, AJ 123, 1389. Dahlem, M., Ehle, M., Jansen, F. et al., 2003, A&A 403, 547. sec2.qxd 7/11/05 5:13 PM Page 18 18 Ehle, M. & Dahlem, M., 2004, Mem. S.A.It. 75, 515. Gondoin, P., Orr, A. & Lumb, D., 2003a, A&A 398, 967. Gondoin, P., Orr, A., Lumb, D. & Siddiqui, H., 2003b, A&A 397, 883. Gondoin, P., Orr, A. & Siddiqui, H., 2004, A&A 420, 905. Guainazzi, M., Rodriguez-Pascual, P., Fabian, A.C., Iwasawa, K. & Matt, G., 2004, MNRAS 355, 297. Harnett, J., Ehle, M., Fletcher, A. et al., 2004, A&A 421, 571. Jimenez-Bailon, E., Piconcelli, E., Guainazzi, M. et al., 2004, A&A, in press. Piconcelli, E., Jimenez-Bailon, E., Guainazzi, M., et al., 2004, MNRAS, 351, 161. Piconcelli, E., Jimenez-Bailon, E., Guainazzi, M. et al., 2005, A&A 432, 15. Schartel, N., Rodriguez-Pascual, P.M., Santos-Lleo, M. et al., 2005, A&A 433, 455. 2.2.4 Ground-based photon-counting studies The SCI-A technology development programme in superconducting detector arrays is being exploited within RSSD. This technology allows for optical photon counting with high efficiency, high time resolution, and photon energy determination, and has been under development for several years. It was last used at the William Herschel Telescope on La Palma in October 2000, resulting in several publications mainly related to the determination of light curves and physical conditions in magnetic Cataclysmic Variables. Papers dealing with temperature determination, and quasar redshift determination, both using the energy-resolved capabilities of the device, have also been published over the last 3 years. The array was recently upgraded from a 6x6 array (S-Cam2) to a 10x12 array (S-Cam3), and operated again at the WHT for six nights in July 2004. The datasets arising from the S-Cam instrument are complex to analyse and interpret. In addition to the issues of photometric stability and calibration of normal CCD cameras (e.g. atmospheric extinction and zenith angle variations) access to the photon arrival times means that the resulting datasets include time-dependent effects (seeing and sky background variations, as well as timedependent differential atmospheric refraction, small amplitude telescope oscillations during short periods of high wind speed, etc) which must be calibrated as part of the pipeline processing. Detector and electronics enhancements made in the development from S-Cam2 to S-Cam3 have resulted in a very stable instrument. A number of different observing programmes, granted through the Netherlands time allocation panel, have been undertaken. Eclipse mapping of three CVs was carried out in a programme led by P. Groot (Nijmijgen). Twelve successive cycles of the 12-min period ultra-compact binary RX J1914+24 were obtained (in a collaboration with G. Ramsay and M. Cropper at MSSL), showing research activities Figure 2.2.4/1: The amplitude of the 10-min orbiter binary RX J1914+24, observed with S-CAM3 in July 2004. Immediately apparent in the colour ratio (bottom panel) are not only the amplitude variation with orbital phase but also the colour dependency of the amplitude. Observations were made in collaboration with Cropper & Ramsey, MSSL (UK). very nice amplitude and colour modulation at the expected period. A series of exploratory observations of pulsating white dwarfs and polar QPOs were undertaken with R. Kotak (Imperial College, London). The high time resolution of the photon arrival time datation (of order a few microseconds) makes the device well suited to the long-running search for further optical counterparts of radio pulsars: one millisecond pulsar and two normal pulsars were observed, under good photometric conditions, with good reference astrometry allowing the expected position of the pulsar to be well centred on the array. Preliminary estimates of the limiting magnitude of these observations, assuming a 10% pulsar duty cycle, are at around V = 26. sec2.qxd 7/11/05 5:13 PM Page 19 research activities 19 2.3 Optical/UV Astrophysics The optical/UV astrophysics research group has relied primarily on HST observations complemented by ground-based facilities to study a wide range of objects, including classical nebulae, the central stars of planetary nebulae, star formation in starburst galaxies and luminous IR galaxies. 2.3.1 The Helix Nebula: when opportunity knocks The Helix Nebula (NGC 7293) lies about 600 ly away in Aquarius and has a diameter of about 2.4 ly, thus spanning as much as 14 arcmin. A substantial portion of the Helix has been imaged in two colours, using both ACS and WFPC2 by N. Panagia and collaborators. Fig 2.3.1/1 shows an image made by combining the new images from the HST-ACS and wide-angle images from the Mosaic Camera on the WIYN 0.9 m Telescope at Kitt Peak National Observatory. This is one of the largest and most detailed celestial images ever made. These HST observations were made possible by a fortuitous combination of events. One of the most prominent meteor showers is the Leonids each November. The shower in 2002 was predicted to be especially rich and since those meteoroids pose a nonzero risk to spacecraft, HST had to carry out a special procedure to minimise the risk and any consequences. As in the past several years, HST was required to point in a particular direction during the meteor shower in order to keep the telescope’s aft end towards the stream, while minimising the cross-section of the solar arrays. This stand-down period was from 0 h to 14 h UT on 18 November 2002. In preparing for this special effort, it was noticed that just outside the nominal pointing region lay the Helix Nebula, which had been imaged by Hubble in some small areas but never in its entirety. This was too good an opportunity to miss! The HST Project at Goddard Space Flight Center was immediately contacted and their concurrence in using HST slightly beyond its nominal pointing area was secured. Thus, it became possible to devote nine orbits of HST observing time to imaging a substantial portion of the large Helix Nebula in two colours, using both ACS and WFPC2, obtaining the most detailed image ever of it. Apart from its outstanding beauty, such an image is also extremely valuable because it is a high-quality first-epoch dataset that is ideally suited for later work on measuring the motions of the tight knots immersed in the nebula. 2.3.2 Central stars of planetary nebulae Stellar evolution predicts that stars in the range 1-8 solar masses will lose most of their stellar envelopes through mass-loss as they ascend the Asymptotic Giant Branch (AGB) phase. It is the mass-loss that establishes the mass Figure 2.3.1/1: The Helix Nebula seen by combining the new images from the HST-ACS and wide-angle images from the Mosaic Camera on the WIYN 0.9 m telescope at the Kitt Peak National Observatory. boundary between those stars that will evolve off the AGB phase into Planetary Nebulae (PNe) and ultimately fade into white dwarfs, and those that will end their lives as type II Supernovae. Studies of Central Stars (CSs) of PNe in the Galaxy are hampered by the poor knowledge of their distances, a problem that can be overcome by observing PNe in the Magellanic Clouds (LMC and SMC; Fig. 2.3.2/1). From ground-based observations, the unresolved nature of the nebula has, however, so far prevented us from taking full advantage of a known distance in the determination of the CS parameters. As a result, most ground-based studies have had to rely heavily on photoionisation modelling of the nebula in order to derive these CS parameters. HST offers a unique opportunity to study the CSs of PNe in the Magellanic Clouds with unprecedented accuracy, largely because the stellar continuum can be measured directly. Villaver and collaborators have determined accurate masses of CSs of PNe for the two largest samples of extra-galactic PNe ever studied, and have explored the connections among the fundamental properties of the stars and the physical properties of the host nebulae (Villaver et al., 2003; 2004). Similar average masses in the LMC and SMC have been established as well as an indication of a difference in the mass distribution of the two samples that cannot be explained by a mass-loss rate dependency with metallicity. As the immediate precursors of white dwarfs, sec2.qxd 7/11/05 5:13 PM Page 20 20 research activities Figure 2.3.2/1: A sample of HST (50 CCD STIS bandpass) images of LMC Planetary Nebulae. From left to right: SMP 4, SMP 10, SMP1 8, SMP 102. The field of view is 3 arcsec and the intensity scale is logarithmic. the study of the mass distribution of the CSs of PNe should help to constrain the initial-to-final mass relation within environments of differing metallicity. 2.3.3 Identifying core-collapse supernovae progenitors With the only exception of type SN Ia, theory predicts that all other types of supernovae arise from the collapse of the core of a massive evolved star that exhausts its nuclear fuel and cannot generate enough energy to support itself. After the explosion of one of these corecollapse supernovae, a neutron star or a black hole is all that remains of the progenitor star. However, there are very few observations of the SN progenitors that can be used to confirm the theoretical predictions regarding their nature. Until 2003, only two SN had had their progenitors unambiguously identified: SN 1987A and SN 1993J. The situation changed that year, when HST played a decisive role in the identification of two new progenitors and in the gathering of new information on one of the previous two. A combination of pre-explosion HST/WFPC2 and Gemini/GMOS images and post-explosion HST/ACS images have been used to identify the progenitor of the Figure 2.3.3/1: Three-colour ACS/HRC mosaic (red: F330W, green: F250W, blue: F220W) of the region around the cluster Sandage 96 in NGC 2403, where SN 2004dj took place, obtained 2 months after the explosion. The field is 90 pc on each side, with north towards the top. The central extended object is the cluster itself (blue owing to the blue giants and supergiants) while the reddish point source is the SN located about 1 pc to the south of the centre of Sandage 96. type II-P SN 2003gd (Smartt et al., 2004). They found that the star was an 8 solar-mass red supergiant, which is consistent with the models of single stellar evolution. Ground-based data from several telescopes have identified that the type II-P SN 2004dj took place in a 14 Myr-old, 24 000 solar-mass stellar cluster that included a number of red and blue supergiants (MaizApellaniz et al., 2004). Post-explosion HST/ACS images obtained by Filippenko et al. were able to resolve the supernova and the surrounding cluster (Fig. 2.3.3/1). Images of the location of SN 1993J with HST/ACS have been obtained that allowed the identification of a bright blue star that could have been the companion of the previously red supergiant that exploded (Maund et al., 2004). The existence of such a companion had been predicted by the theoretical models that had been sec2.qxd 7/11/05 5:13 PM Page 21 research activities advanced to explain the peculiar evolution of the SN, which started out as a hydrogen-rich type II to later transform into a helium-rich type Ib. 2.3.4 Metals in the dwarf starburst galaxy NGC 1705 NGC 1705 is one of the most intriguing nearby objects. At a distance of 5 Mpc, it is a dwarf galaxy that is experiencing intense star formation, a so-called starburst. As a result, it hosts in its centre a compact and massive young star cluster and shows evidence of a spectacular large-scale outflow triggered by the simultaneous explosion of a myriad of SNe II. The extreme physical conditions of starbursts like NGC 1705 must have been much more common in the past, making them crucial targets against which observations of higher-redshift galaxies must be compared. 21 the starburst environment. What we observe could thus be the result of either chemical pollution of the medium closely surrounding the starburst or a metallicity gradient from the inner metal-rich galaxy to an outer metal-poor halo. The metal offset between the neutral and ionised ISM has important implications for the chemical evolution of dwarf starburst galaxies, since it implies that widespread enrichment episodes have preceded the current burst that dominates the bolometric luminosity of these systems. A potential scenario is one where star formation dates quite far back in the past, allowing the metals to be produced in the most central regions and efficiently dispersed in the surrounding neutral gas of the halo. The ISM non-homogeneity may also imply a larger loss of metals via galactic winds than previously thought, thus favoring ‘bursty’ over low-level quasi-continuous star formation. 2.3.5 Luminous IR galaxies: a key galaxy population Dwarf starburst galaxies are characterised by a large reservoir of neutral gas. This is a fundamental ingredient for the star-formation onset, but it is also the place where most of the baryons may hide. A. Aloisi and collaborators have studied the neutral ISM of NGC 1705 by analysing the absorption lines detected in highresolution UV spectra of its central cluster. The synergy between the complementary spectral ranges of the HST/STIS and FUSE data used in this project has allowed for the first time the issues involved in this type of analysis (e.g., saturation, ionisation and depletion) to be tackled. The study shows that the metals abundance in the neutral gas of NGC 1705 are lower than in the ionised gas of the H II regions probed via optical nebular spectroscopy. This intriguing result unambiguously indicates that the ISM in dwarf star-forming galaxies is not homogeneous as previously suggested and usually assumed in chemical evolution models, and may imply the existence of a lower metallicity halo that surrounds Luminous IR Galaxies (LIRGs) are believed to be very common in the distant Universe, and are probably the local counterpart of the sub-mm galaxies that give rise to the far-IR background. The physical processes at work in LIRGs (mergers of galaxies, dust-shrouded massive starbursts, AGN formation, outflows, enrichment of the intergalactic medium, etc) are likely to be the same as in young galaxies in the early Universe. Therefore, they are natural laboratories for understanding these processes in detail, providing a local reference to high-z galaxy population studies. A project aimed at studying the internal structure and kinematics of a representative sample of LIRGs is underway. This study is based on Integral Field Spectroscopy (IFS) using the 4.2 m William Herschel Telescope and HST imaging (WFPC2 and NICMOS). These two techniques are ideal and complementary to study the complex physical and kinematics properties of these objects. The analysis is mainly based on the rest frame optical spectral diagnostic features (and near-IR morphologies), which will be shifted towards longer wavelengths in the high-z galaxy populations to be studied with JWST. Furthermore, the linear resolutions to be obtained with JWST for high-z populations are coarsely of the order of those now obtained from the ground for local LIRGs. Figure 2.3.5/1: HST/NICMOS (K-filter) image of the ultra-luminous IR galaxy IRAS 17208-0014, likely a merging of two galaxies in its final dynamical phase. The iso-contours indicate the ionised gas (H-alpha) velocity dispersion map (top) and velocity field (bottom) obtained with the fibre system on the 4.2 m WHT. sec2.qxd 7/11/05 5:13 PM Page 22 22 Figure 2.3.5/1 presents the ionised gas (Hα) velocity dispersion map and velocity field of IRAS 17208-0014 (iso-contours), together with the near-IR image obtained with HST/NICMOS (Arribas & Colina, 2003). It is interesting to note that the peak of the velocity dispersion map is centred on the near-IR continuum maximum, which indicates that for this galaxy the velocity dispersion seems to be a good mass tracer. Furthermore, the velocity field has a pattern compatible with rotation, with its kinematical centre in positional agreement with the nucleus. This is a surprising result and differs from those obtained for most of the objects studied so far, where the velocity fields are rather dominated by tidal induced forces. If velocity fields do not show rotation they cannot be used for obtaining dynamical masses, a key observational parameter for testing the hierarchical models of galaxy formation and evolution – these models predict an increase of galaxy masses over cosmic time. If velocity fields cannot be used for inferring dynamical masses, such models have to be tested by more indirect techniques. References Arribas, S., Colina. L., 2003, ApJ 591, 791. Maiz-Apellaniz, J. et al., 2004, ApJL (10 November 2004 issue). Maund, J.R. et al., 2004, Nature 427, 129. Smartt, S.J. et al., 2004, Science 303, 499. Villaver, E., Stanghellini, L. & Shaw, R.A., 2003, ApJ 597, 298. Villaver, E., Stanghellini, L. & Shaw, R.A., 2004, ApJ 614, in press. research activities 2.4 Infrared/Sub-millimetre Astrophysics The research group continues to utilise the ISO archive extensively to further its research interests in a wide range of astronomical topics, ranging from Solar System studies to analysis of deep fields. 2.4.1 Solar System studies Salama, together with Coustenis et al., has continued the analysis of the ISO Titan data taken by the SWS instrument. The near-IR spectra of Titan show several weak CH4 absorption regions, in particular centred near 2.75 µm. Owing to interference from telluric CO2 absorption features, only part of this region (2.9-3.1 µm) has been observed from the ground. ISO observations show the 2.75 µm window in its full shape for the first time. Using a detailed microphysical model of Titan’s atmosphere, information on the atmospheric parameters (haze extinction, single scattering albedo, tholin refractive index, etc.) has been derived by fitting the methane bands. From the derived surface albedo spectrum around 2.75 µm, some constraints on Titan’s surface composition were determined. ISO data appear to be compatible with H2O and CO2 ices. 2.4.2 Interstellar medium studies Work has progressed on the study of the dust emission of the interstellar medium of our Galaxy with balloon-borne sub-mm data (Dupac et al., 2003a) as well as with largescale space-borne measurements. In addition, the dust emission of the NGC 891 galaxy was studied (Dupac et al., 2003b). This research was performed in collaboration with the Cold Universe group of CESR in Toulouse (F). In addition, the analysis of the Archeops balloon-borne experiment data, notably concerning the first detection of polarisation of the submillimetre dust emission (Benoit et al., 2004) and the measurement of the dust temperaturepolarisation spectrum is ongoing. This work includes the measurement of the harmonic spectrum of the Cosmic Microwave Background fluctuations. In addition, in preparation for the Planck satellite operations phase, simulations of different scanning strategies for the cosmic microwave background is underway (Dupac & Tauber, 2005). Studies continue with CESR (Toulouse) into the gas/grain interaction in quiescent-dense interstellar medium (a filament in Taurus), using molecular lines and continuum tracers. Studies of the dust properties in nine interstellar regions have also been fruitful, mostly from ISO observations at 60-200 µm (del Burgo et al., 2003), where an increased far-IR emissivity was observed in big dust grains (15110 nm) towards low temperatures. The relative abundance of very small grains (1.2-15 nm) with respect to the big grains shows significant variations from region sec2.qxd 7/11/05 5:13 PM Page 23 research activities 23 Figure 2.4.2/1: CVF observation of the M31 bulge. Top: corrected images at 6 µm and 11.3 µm and, for comparison, the uncorrected 11.3 µm image. Bottom: spectrum of the M31 bulge obtained by linearly correlating the smooth radial gradient of the bulge emission at each wavelength with that measured at 6 µm (left), and the spectrum of the dust clouds that can be seen in the images (right). to region at low column densities. Along lines of sight of higher column density, the data indicate the disappearance of small grains. These results can be interpreted in terms of coagulation of dust. The larger size and porous structure of grains could explain the increased far-IR emissivity. The far-IR emission from large grains in Taurus has been separated into warm and cold components, from which the temperature and optical depth of the components was determined and compared with the properties of the molecular gas. In addition, characterisation of the cirrus structure over the 90200 µm wavelength range continues (Kiss et al., 2003). proto-Oort cloud at distances of several tens of thousands of AU from the binary. Improvements in the data reduction of the ISOCAMCVF have been made that were motivated by the goal of analysing extended emission data in less excited regions of the sky. The key features of the new data process are the subtraction of the zodiacal emission and the associated straylight, the improvement of the wavelength calibration, and the astrometry. The scientific information that can be now extracted from the data is greatly enhanced for the large number of observed fields with extended emission fainter than the zodiacal light. Thanks to all these corrections, reliable spectrum and spatial structure of extended objects can be extracted. The results of the improved pipeline have been made available for public use in the ISO archive. As part of the GLIMPSE legacy team of the NASA Spitzer Space Telescope, a survey has been conducted of parts of the Galactic Plane in four IR wavebands between 3.6 µm and 8 µm. The early results of protostars in the Elephant Trunk Nebula and the discovery of a distant star-formation region have been published by Reach et al. (2004) and Mercer et al. (2004), respectively. 2.4.3 Star formation The investigation of the star-forming system in L1551 has continued. It is now clear that the inner parts of this proto binary (class 0/1) is surrounded by a massive (> several solar masses) disc, from which the outflow lifts off. Aspects of the shocks within the outflow are being investigated, particularly with respect to the recently discovered X-ray source. In addition – for the first time – methanol from the outer edges of this disc has been detected, which suggests that it could be due to a Analysis of a sample of high-luminosity star-forming regions observed by ISO LWS indicate they are characterised by strong far-UV stellar fields causing atomic ionisation. This work has shown how photoionisation models can explain the observed fine structure line luminosities and where other components, such as photodissociation emission and shock excitation by outflows, have to be included to account for the observed spectra. Two research projects concerning low-mass brown dwarfs and planetary-mass objects in star-forming regions are also underway. The first is based on very deep ISOCAM images of the Taurus molecular cloud. The IR excess from the circumstellar disc of the forming stars is commonly used to identify young stars. It has been found that, in contrast to previous studies in which the presence of galaxies in the field was not taken into account, the galaxies dominate the detections at these low flux-levels. These results have ramifications for the interpretation of the deep images of star-forming regions acquired by the Spitzer Space Telescope. The second project compares two different methods for identifying young stars. In general, mid-IR studies yield a higher fraction of low-mass stars when compared to optical and near-IR surveys. The questions addressed are: ‘What is the cause of this discrepancy?’ and ‘Which method gives the best measure of the true fraction of sec2.qxd 7/11/05 5:13 PM Page 24 24 low-mass objects?’. Highly embedded regions (i.e. regions with very recent star formation) are best studied in the mid-IR because of the large extinction. This extinction may cause a strong bias in optical studies. For older regions, optical surveys bring the advantage of increased sensitivity and higher spatial resolution. The Chamaeleon star-forming region is the ideal intermediate in which both methods have been applied. The candidate lists from both mid-IR (ISOCAM) and near-IR surveys have been compared. They find that the effects of extinction in the optical are minimal and only a few stars in the very densest part are undetected in the near-IR survey. Investigations into aspects of the process of star- and solar system-formation have continued. High-resolution spectra have been obtained with the VLT/UVES combination of the Beta Pictoris disc. The data maps the gas distribution within the gas disc in more than 70 absorption lines, demonstrating the warping of the disc. Gas can be traced from the inner parts out to more than 400 AU. The origin of the gas remains unclear; the investigation clearly shows that the gas is not accelerating outwards as it should do, given the radiation pressure. An unseen molecular component may hold the atomic gas in place. 2.4.4 Stellar studies A local interface dynamo model has been developed in order to reproduce the activity cycles of about 30 Suntype stars, which have been detected by monitoring, since 1966, the photometric variation in two bands centred in the Ca II H and K lines. The local model splits the dynamo equations into two systems, the first for the overshoot region where the strong toroidal field is assumed to be produced by the internal differential rotation, and the second for the base of the convection zone where the so-called alpha-effect produces the poloidal field. The model includes some new features, such as the refraction of the magnetic waves from the overshoot region to the convection zone, and the scaling of the width of the shear layer where the differential rotation is concentrated in the Sun. The observed trends in the magnetic cycle and rotation periods are well reproduced by the model. The dependence of the magnetic intensites in the stellar interiors on the spectral types, obtained with the model, agrees with that followed by the observed surface magnetic fields. Nova continue to be studied through the use of observations made by ISO SWS. For CP Crucis (Nova Crux 1996), abundance enhancements versus solar by mass were found to be of 75, 17 and 27 for N, O and Ne, respectively, from ISO and quasi-simultaneous groundbased observations. Additionally, the Mg abundance in the ejecta is constrained to be approximately solar. The nova appears to be an example of the ‘missing link’ research activities between CO and ONeMg novae (Lyke et al., 2003). For Nova V723 Cassiopae, the IR spectrum was dominated in the first year by H and He recombination lines, and at later times by coronal lines. From the H recombination lines, electron temperature and an electron density were derived. From the coronal lines abundance ratios of S/Si ≈ 2.1, Ca/Si ≈ 1.6 and Al/Si ≈ 1.5 were found. The ejected mass was also constrained (Evans et al., 2003). ISO/SWS IR spectra of oxygen-rich AGB stars with optically thin dust shells continue to be exploited (Heras & Hony, 2005). The low mass-loss rate regime is of particular interest because, owing to the low densities of the outflow, dust condensation may not be complete and it is possible to observe the intermediate steps in the dust condensation sequence. The composition of the dust and the physical conditions in the shells were determined by modelling the SWS observations with the radiative transfer code DUSTY. Through the comparison with the CO observations found in the literature, gas-to-dust ratios were calculated and the mass-loss rates derived. The results show that, even in the low-density environments studied, the dust produced is enough to drive the stellar wind by radiation pressure. The composition of the dust and its dependence on the physical conditions at the inner shell is consistent with the thermodynamic dust condensation sequence. However, the temperatures derived for the dust formation are lower than those estimated by current theories. ISO/SWS spectra of S stars are also now being examined. These AGB stars have abundances between the oxygen-rich and the carbon-rich AGB stars. Owing to this intermediate composition pattern, the molecules and solid components that form around such stars are poorly known. In general, it is assumed that the solid particles are predominantly silicates, i.e. oxygen-rich dust. The new ISO spectra present the first-ever detection of magnesium-sulphide grains around S stars. Such grains are otherwise observed only in carbon-rich environs. Furthermore, the spectra indicate that the silicates present around these stars are systematically different from those found around oxygen-rich AGBs. A radiative transfer model has been developed in order to derive physical parameters (size, distance, density) of detached dust shells around carbon-rich AGB stars based on their IR spectra (Hony & Bouwman, 2004). This model was also applied to two well-studied stars with good agreement with other methods (CO mapping and imaging of light scattered from the dust). The new method can be easily applied to more distant stars where these other techniques fail. It is intended to apply and test the new model extensively by using new observations from the Spitzer Space Telescope in three accepted programmes. Studies of the dust shell around the peculiar post-AGB object HD 56126 (Fig. 2.4.4/1) have also been sec2.qxd 7/11/05 5:13 PM Page 25 research activities 25 merging of multiple observations of the same source, about 16 500 mid-IR objects were confirmed with a confidence level of the detection probability to better than 99%. The catalogue will contain these sources and associated flags like source characterisation, detection quality and astrometric correction. The typical sensitivity limit reached in this survey is about 1 mJy, with a median of 3.9 mJy. Figure 2.4.4/1: Multi-wavelength spectrum of the post-AGB object HD 56126. The star is surrounded by a shell of carbon-rich dust. The shell is easily identified in the mid-IR image (top-left), while the star itself (indicated by the star symbol) is hardly detected. The spectrum is clearly divided in two components; the star dominates the UV and optical light, while all the IR radiation originates from the dust in the shell roughly 2500 AU away. The various dust components have been indicated. conducted (Hony et al., 2003). From the detailed radiative transfer modelling of the IR spectrum and imaging, stringent constraints are placed on the composition and physical parameters of the shell. It has been found that the star has relatively normal dust properties but has exhibited an atypically high mass-loss rate. The analysis of individual stellar sources evolving from the AGB to the PN stage, using multi-wavelength observations, has continued. In particular, in collaboration with A. Riera (U. Barcelona) and others, a detailed analysis was made of the remarkable highly collimated optical jets associated with the proto-PN Hen 3-1475 (Garden Sprinkler Nebula), interpreted as the result of episodic mass loss by a precessing binary system. A detailed chemical abundance analysis of the PN Me 2-1 was also carried out using a combination of ISO and IUE data, with optical spectra taken from the literature. Finally, two rare, new type I PNe belonging to the Galactic Bulge population were identified as such and studied in detail. 2.4.5 Extragalactic studies The ISOCAM Parallel Mode observations continue to be exploited. A 27 sq. deg. area was observed with LW2, a broadband filter centred on 6.7 µm. The work on the resultant point source catalogue is close to completion: after statistical cleaning, astrometric corrections and As a first scientific result derived from ISOCAM parallel results, a collaboration led by Haas (Ruhr Universitaet Bochum, D) discovered unique mid-IR excess sources. Various arguments suggest that they likely contain an AGN. The ongoing optical spectroscopy indicates 40% of the sample to be classical AGN and the remaining part to be dust-shrouded sources. A survey of mid-IR selected AGNs was initiated to confirm this. In addition, observing time was granted by Spitzer and TNG. Improvements in the ISO calibration has led to further work in the areas of the far-IR source count analysis and luminosity function in the ELAIS fields (Heraudeau et al., 2004; Serjeant et al., 2004) and cosmic far-IR background (Rowan-Robinson et al., 2004). A series of papers on the deep ISOCAM survey through gravitationally lensing galaxy clusters has been published. Metcalfe et al. (2003) presented the catalogue of 7 µm and 15 µm observations of 148 midIR sources from the A370, A2218 and A2390 fields. The fluxes of lensed background sources were corrected for amplification to yield source counts reaching three times deeper than other mid-IR surveys. These counts confirmed and extended earlier findings of a factor of ten excess of 15 µm galaxies compared to models with no evolution. Most sources occur at 0.4 < z < 1.5 with median ~0.6, and resolve the bulk of the cosmic mid-IR background. Clusters of galaxies have also been studied (Biviano et al., 2004; Coia et al., 2005a; 2005b) based on archival and published data to investigate the properties of clusters of galaxies over a range of redshift (0.18 < z < 0.4). Clusters A2219, Cl0024+1654 and A1689 were included, for a total sample of about 75 cluster sources, constituting a substantial fraction of the ISO results on galaxy clusters beyond Virgo and Coma. Comparing IR-based star-formation rates with optical results shows up to 90% of cluster star-formation activity hidden from optical spectra by dust. Clusters were compared at 15 µm. Cl0024 has similar redshift to A370 but hosts ten times as many luminous IR galaxies (LIRGs). No LIRGs were detected in A1689, A2218 or A2390, while a total of three might have been expected based on the results from Cl0024. The sources in Cl0024 are much more powerful than those in A1689 and A2218. A2218 galaxies were fitted by models of quiescent ellipticals. The 13 galaxies detected in Cl0024 are strongly star-forming. sec2.qxd 7/11/05 5:13 PM Page 26 26 References Benoît, A., Ade, P., Amblard, A., et al., 2004, A&A 424, 571. Biviano, A., Metcalfe, L., McBreen, B., et al., 2004, A&A 425, 33. Coia, D., McBreen, B., Metcalfe, L. et al., 2005a, A&A 431, 433. Coia, D., Metcalfe, L. McBreen, B., et al., 2005b, A&A 430, 59. del Burgo, C., Laureijs, R. J., Ábrahám, P., Kiss, Cs., 2003, MNRAS 346, 403. Dupac, X., Bernard, J.-P., Boudet, N., et al., 2003a, A&A 404, L11. Dupac, X., del Burgo, C., Bernard, J.-P., et al., 2003b, MNRAS 344, 105. Dupac, X. & Tauber, J., 2005, A&A 430, 363. Evans, A., Gehrz, R.D., Geballe, T.R., et al., 2003, AJ 126, 1981. Héraudeau, Ph., Oliver, S., del Burgo, C., et al., 2004, MNRAS 354, 924. Hony, S., Bouwman, J., 2004, A&A 413, 981. Hony, S., Tielens, A.G.G.M., Waters, L.B.F.M., de Koter, A., 2003, A&A 402, 211. Heras, A. & Hony, S., 2005, A&A, in press. Kiss, Cs., Ábrahám, P., Klaas, U., et al., 2003, A&A 399, 177. Lyke, J.E., Koenig, X.P., Barlow, M.J., et al., 2003, AJ 126, 993. Mercer, E.P., Clemens, D.P., Bania, T.M., et al., 2004, ApJS 154, 328. Metcalfe, L., Kneib, J.-P., McBreen, B., et al., 2003, A&A 407, 791. Reach, W.T., Rho, J., Young, E., et al., 2004, ApJS 154, 385. Rowan-Robinson, M., Lari, C., Perez-Fournon, I., et al., 2004, MNRAS 351, 1290. Serjeant, S., Carramiñana, A., Gonzáles-Solares, E., et al., 2004, MNRAS 355, 813. research activities 2.5 Solar Physics The research group continues to use SOHO observations extensively to further its research interests in a wide range of topics in solar physics, such as studies of the chromosphere, transition region dynamics and coronal magnetic fields. 2.5.1 Chromospheric oscillations Investigations are underway to study the interaction of the topographic structure of the solar chromospheric plasma with the wave modes observed (McIntosh & Fleck, 2004; McIntosh et al., 2003). A distinct correlation between the inferred plasma topography and the phase differences between and suppression of oscillations at different levels in the solar atmosphere has been established (Fig. 2.5.1/1). This can be interpreted as evidence of interaction between the waves and the extended magnetic ‘canopy’. Coronal holes are the lowest density plasma components of the Sun’s outer atmosphere. They are associated with rapidly expanding magnetic fields and are the source regions of the fast solar wind. The interfaces between open and closed regions make them a topologically interesting place. McIntosh et al. (2004) have therefore studied the propagation characteristics of chromospheric oscillations in and around an equatorial hole by applying phase-difference and travel-time diagnostics to TRACE time series in the 1700 Å and 1600 Å UV continua bandpasses. Their results suggest a significant change in atmospheric conditions at the base of the chromosphere inside the coronal hole relative to its boundary and quietSun regions. Fig 2.5.1/2 shows a SOHO EIT 195 Å context image from 2003 July 14, 00:08 UT. The TRACE field-of-view is shown as the thick red rectangular region. The coloured contour levels qualitatively indicate the coronal hole boundary. Figure 2.5.1/3 shows a travel-time map between the 1700 Å and 1600 Å signal. The travel-time (∆t) at any frequency (ν) is computed by applying a Gaussian filter, G(ν, δν), about ν with a width δν to each bandpass, cross-correlating the two filtered sequences and determining the shift of the cross-correlation function. The 1700 Å continuum is formed a few tens of km below the 1600 Å continuum. For upward travelling waves, the 1700 Å signal therefore leads the 1600 Å signal by a few seconds (negative travel-time according to the convention applied here). There is a notable difference in travel-time between the coronal hole interior and exterior (~4 s). Interpreting the waves as being predominantly acoustic in nature, the observed travel-time, ∆t ≈ ∆z/cs, is directly proportional to the height difference between the two bandpasses, where cs is the local sound speed in the lower sec2.qxd 7/11/05 5:13 PM Page 27 research activities 27 Figure 2.5.1/2: SOHO EIT 195 Å context image from 2003 July 14, 00:08 UT. The red rectangular region shows the TRACE field-of-view, while the yellow and orange contours show the 100 DN and 200 DN intensity levels in the image, respectively. Figure 2.5.1/1: Upper left: spatial variation in the altitudes at which the plasma-β is of order unity in the TRACE field of view. Solid contours are added for reference, each separated by 0.25 Mm. The map is based on a potential field extrapolation of a timeaverage MDI longitudinal magnetogram. The presence of the network elements, where the βtransition height is blue-violet in colour, is perhaps the most striking feature. The other panels show one example of the integrated oscillatory power in the 38 mHz band of the 1700, 1600 and 1550 Å TRACE UV bandpasses, respectively. On each of these panels we have overplotted the contours of the β-transition height in the upper left. Note the clear correlation between the reduced power and the contours. chromosphere (~6 km/s). For a filter frequency of 7 mHz, the 4 s difference can therefore be approximated to a difference in ∆z of 24 km between the coronal hole interior and its boundary, a not insignificant fraction of a scale height near the chromospheric temperature minimum (~100 km). This is a quite unexpected and confounding result: Why would the largely hydrodynamic (high plasma-β) coronal hole interior plasma at the base of the chromosphere care Figure 2.5.1/3: Travel-time map at full TRACE resolution between the 1700 Å and 1600 Å bandpasses. The coloured rectangles denote regions of coronal hole interior (red), coronal hole boundary/exterior (blue), and coronal hole arcade (purple). sec2.qxd 7/11/05 5:13 PM Page 28 28 about the fact that the magnetic field is open to the interplanetary medium and stratify itself so? Conventional thinking would assume that the chromosphere should have little knowledge of the topologically open coronal holes above. Follow-up studies addressing a possible connection between the mixture of field polarities, proportion of open/closed magnetic structures, UV/EUV intensity/Doppler velocity contrast, and in situ solar wind measurements are ongoing. 2.5.2 Dynamics of transition region blinkers Blinkers are small-scale intensity enhancements observed in the transition region of the solar atmosphere. They were first detected by eye in SOHO/CDS data, but automated methods have been developed more recently to identify these events. Blinkers are best observed in O V (which is formed at a temperature of 2.5x105K) and have mean areas of 3x107 km2 and mean lifetimes of 16 min. They are either density enhancements or increases in filling factor, but not temperature events. They occur above regions where one polarity of magnetic field dominates, including quiet Sun, plage regions or sunspots. Such blinkers can be further investigated by studying the relative Doppler and non-thermal velocities of quiet-Sun and active-region blinkers identified in O V with SOHO/CDS. It has been found that O V blinkers have a preference to be more redshifted than the normal Figure 2.5.2/1: Three SOHO/CDS O V rasters taken 7 min and 8 min apart. The circled region shows a blinker in the second frame. research activities transition region, but the range of these enhanced velocities is no larger than the typical spread of Doppler velocities in this region. The anticipated ranges of Doppler velocities of blinkers are 25-30 km/s in the quiet Sun (20-40 km/s in active regions) for O V. Bewsher et al. (2003) also found that blinkers have preferentially larger non-thermal velocities than the typical background transition region. Again, the increase in magnitude of these non-thermal velocities is no greater than the typical ranges of non-thermal velocities. The range of non-thermal velocities of blinkers in both the quiet-Sun and active-regions are estimated to be 3045 km/s in O V. There are more blinkers with larger Doppler and nonthermal velocities than would be expected in the whole of the transition region. The results have been used to help elaborate further the many mechanisms proposed to explain blinkers. 2.5.3 Comparison of blinkers and explosive events Blinkers (intensity enhancements) are predominantly observed with the CDS instrument on SOHO and were discussed in the subsection above. Explosive events, however, are characterised by strong non-Gaussian enhancements in the wings of spectral lines, and have large velocities (50-250 km/s) associated with them. Explosive events have recently been observed with the SUMER instrument on SOHO but where first observed using HRTS. They have a mean area of 1 Mm2 and mean lifetime of 1 min. They are associated with regions of complex weak fields or on the edges of unipolar. Models of the magnetic reconnection configuration required for explosive events to occur have also been presented. There has been much speculation as to whether blinkers and explosive events are the same phenomenon, but observed differently with the CDS and SUMER instruments. Bewsher et al. (2004a) have analysed co-spatial and co-temporal CDS and SUMER datasets and automatically identified both blinkers and explosive events in both instruments data. They found that blinkers were identified in the SUMER data if the temporal resolution of the data was reduced to that of the CDS data, otherwise short-lived localised intensity enhancements were identified. Explosive events were identified in the CDS data if the width of the spectral line was significantly increased, and occasionally if an enhancement in the wing was present. In 3.5 h of data, they found only one case where a blinker and an explosive event coincided, ten examples of lone blinkers and seven examples of lone explosive events. This has sec2.qxd 7/11/05 5:13 PM Page 29 research activities (a) 29 Figure 2.5.3/1: (a) SUMER single slit image showing an explosive event labelled S1; (b) CDS raster showing blinkers labelled C1-3. The diamonds on the CDS raster mark the locations of blinkers and the vertical dashed line indicates the position of the SUMER slit. (c-d) lightcurves of the explosive event, S1 and blinker, C2 (which is closest spatially to the explosive event). (e-f) spectral line profiles of the explosive event S1 and blinker C2. (b) (c) (d) Figure 2.5.4/1: Highly twisted magnetic flux tube inside an active region obtained from a non-linear force-free extrapolation technique based on photospheric vector magnetograms. The contours characterise the vertical magnetic field strength on the photosphere. (e) (f) led to the suggestion that blinkers and explosive events are not the same type of event. A theoretical statistical model was presented in Bewsher et al. (2004b), which hypothesised that blinkers and explosive events are random and not physically connected in any way. 2.5.4 Coronal magnetic fields To understand most of the phenomena in the solar corona, such as flares, CMEs and filament eruptions, knowledge of the 3-D magnetic field is required. Considering that the observed solar region is in a forcefree equilibrium state, the coronal magnetic field can be extrapolated from photospheric magnetic field measurements. Régnier and co-workers used vector magnetograph measurements to study magnetic structures inside active regions (filaments or sigmoids) and their evolution before and after flares. Régnier & Amari (2004) have found that a filament and a sigmoid can both be described by a twisted flux tube with a number of turns less than 1 and opposite electric current densities. They have also shown that the eruption associated with the studied active region is most likely due to a highly twisted flux tube with a number of turns more than 1 (Fig. 2.5.4/1) different from the filament and the sigmoid. Studying the dynamics of an active region has also shown that the main progenitors of small flares sec2.qxd 7/11/05 5:13 PM Page 30 30 research activities identification of the source of the flare at a reversed-Y null point in the low corona. Figure 2.5.4/2: Characteristic magnetic configuration of the active region where most of the flares of October/November 2003 originate. Red field lines describe the system of loops involved in the post-flare phenomena. The background image is the SOHO/MDI magnetogram at 10:00 UT Oct 28, 2003. in an active region are the transverse photospheric motions (sunspot rotation, magnetic flux emergence) and the complex topology (separatrix surfaces, separators) (Régnier & Canfield, 2004). The extrapolated coronal magnetic configurations are used to construct the synthetic X-ray and EUV emission maps by solving the energy equation along each individual coronal loop (Lundquist et al., 2004). The constructed maps are compared with observed images recorded by Yohkoh/ SXT and SOHO/EIT, giving some constraints on the coronal heating mechanism. Vector magnetograms are also useful for determining the flow field on the photosphere. By combining the induction equation and the local correlation technique, Welsch et al. (2004) were able to self-consistently derive the three components of the flow field at the photospheric level. The flow fields as well as the forcefree coronal magnetic configurations are the boundary conditions of magnetohydrodynamic (MHD) evolution codes. Over 2 weeks in October/November 2003, the Sun featured unusually strong activity, with 12 X-class flares and two significant proton storms. Régnier & Fleck (2004) studied the magnetic properties of AR 10486 (the active region in which most of the events occurred) before and after the X17.2 flare on 28 October. Two methods were used: (i) the study of the active region dynamics by determining the potential coronal field from SOHO/MDI magnetograms with a high temporal cadence, as shown in Fig. 2.5.4/2; (ii) the analysis of a more accurate coronal magnetic configuration using a non-linear force-free extrapolation from a vector magnetogram taken before the flare, which led to the References Bewsher, D., Parnell, C.E., Pike, C.D., Harrison, R.A., 2003, Solar Physics 215, 217. Bewsher, D., Innes, D.E., Parnell, C.E., Brown, D.S., 2004a, A&A, submitted. Bewsher, D., Brown, D.S., Innes, D.E., Parnell, C.E., 2004b, ESA SP-575, 465. Lundquist, L.L., Fisher, G.H., McTiernan, J.M., Régnier, S., 2004, ESA-SP 575, 306. McIntosh, S.W. & Fleck, B., 2004, ESA SP-547, 149. McIntosh, S.W., Fleck, B., Judge, P.G., 2003, A&A 405, 769. McIntosh, S.W., Fleck, B., Tarbell, R.D., 2004, ApJ 609, L95. Régnier, S. & Amari, T., 2004, A&A 425, 345. Régnier, S. & Canfield, R.C., 2004, ESA-SP 575, 255. Régnier, S. & Fleck, B., 2004, ESA-SP 575, 519. Welsch, B.T., Fisher, G.H., Abbett, W.P., Régnier, S., 2004, ApJ, 610, 1148. sec2.qxd 7/11/05 5:13 PM Page 31 research activities 31 2.6 Heliospheric Physics/Space Plasma Studies The scientists in SCI-SH have expertise in the observations of electromagnetic fields and plasma particles, as well as in the detection of high-energy particles. Basically, their studies deal with two major areas. Firstly, how the solar wind originates and how it varies in the heliosphere; the team has particular expertise in solar energetic particles in the MeV range. Secondly, how the Earth’s plasma environment (the magnetosphere and ionosphere) is driven by the solar wind, particularly the transfer of particles between different regions as well as how particles are energised in the magnetosphere. 2.6.1 Energetic particles from the October/ November 2003 solar events The research group has investigated heliospheric effects of the intense solar activity that occurred in OctoberNovember 2003 using observations of the COSPIN/LET instrument on the Ulysses spacecraft located near the solar equator at 5.2 AU from the Sun. COSPIN/LET was built by members of SCI-SH together with current members of SCI-A. Figure 2.6.1/1 (top panel) presents the proton/alpha ratio for the 42-day period after 17 October (DOY 290). Dashed vertical lines mark the times of forward (F) and reverse I shocks identified in the magnetic field data at Ulysses, where F-shocks labelled in red indicate probable CME-driven shocks. The lower panel contains heavy ion abundance ratios (1-day averages), all normalised to the solar energetic particle (SEP) composition. Shown for reference is the 1.2-3.0 MeV proton intensity. The onset time and duration of a large CME associated with the October-November 2003 activity is marked by an inverted triangle. Solar wind conditions at Ulysses prior to the period of enhanced solar activity were dominated by recurrent high-speed/low-speed stream interaction regions (SIRs). As a result of the increased activity, and the associated CMEs, this pattern was temporarily disrupted. The highest particle intensities occur at the time of the reverse shock on DOY 314/10 November, although the preliminary analysis does not allow us to determine conclusively whether or not this is the result of local acceleration of the pre-existing SEP population. With the possible exception of He, which apparently shows a typical corotating interaction region (CIR) enhancement (decrease in p/He, increase in He/O), the composition signatures suggest that the CIR reverse shock processed the ambient SEP population (as evidenced by the SEPlike C/O ratio). If real, the enhanced He content within the CIR is presumably the result of accelerated interstellar pickup helium. The signature for Fe/O is suggestive of CIR composition, but very large scatter in daily values prevents a firm conclusion. Figure 2.6.1/1: Energetic particle observations of the COSPIN/LET instrument on Ulysses. 2.6.2 Energetic particles in the high-latitude, highspeed solar wind A detailed study has been made of energetic particle events observed by COSPIN/LET during the recent second northern polar pass. For a short time during this high-latitude pass, Ulysses was immersed in high-speed solar wind from the newly formed northern polar coronal hole. Four large SEP events were observed, permitting significant conclusions to be drawn concerning the propagation of the particles to high latitudes. A topic of considerable debate triggered by Ulysses observations is the role played by perpendicular diffusion in the transport of charged particles in the heliosphere. Based on the events studied here, no evidence has been found for local transport across the magnetic field. Indeed, the particle angular distributions at the onset at all energies were considerably more isotropic than events seen at lower latitudes, or even at 1 AU. It must be stressed that the observations do not allow conclusions to be drawn about particle propagation close to the Sun. Even though, at the location of Ulysses, particles were propagating along the magnetic field lines and not across them, there may be cross-field diffusion occurring close to the solar surface. Another possible mechanism is the large-scale distortion of the magnetic field connecting Ulysses to the Sun at lower latitudes by, for example, an outward-moving coronal mass ejection. Continuing the research group’s study of the relationship between the Sun and the heliosphere, the group is sec2.qxd 7/11/05 5:13 PM Page 32 32 research activities involved in a new instrument for NASA’s STEREO spacecraft. The instrument comprises a proton and electron telescope. Staff from SCI-A designed, manufactured and tested the overall electronics for the SEPT instrument for two NASA/STEREO satellites; the electronics is highly miniaturised using ASIC components. The instruments have been delivered for final testing at Caltech. The PI institute of the instrument is the University of Kiel (D); SCI-SH Co-I’s are R. Marsden and T. Sanderson. 2.6.3 Acceleration of electrons in the auroral region One of the key issues in space plasma physics is the acceleration of charged particles. In the auroral region, electrons become highly accelerated before hitting the Earth’s atmosphere and causing auroral emission. The acceleration is often related to the occurrence of large electric fields, either DC or wave electric fields, which can be monitored with electric field instruments. The NASA Polar satellite (1996-) carries such an instrument that was in part built by the SCI-SH team together with current members of SCI-A. Figure 2.6.3/1, taken from Janhunen et al. (2004c), provides one possible approach to the acceleration processes occurring in the auroral region. It appears that an island of density cavities (see the isocontours in the figure) and enhanced electric field structures occur at 45 RE radial distance in the evening and midnight magnetic local time (MLT) sectors in the auroral region during disturbed conditions. At the same time, the ion beam occurrence frequency changes at the same altitude (these ions come from the Earth’s atmosphere). It is proposed that the mechanism involved in the electron acceleration is electron Landau resonance with incoming Alfvén waves. The auroral kilometric radiation (AKR) is the strongest electromagnetic emission generated around the Earth and it can be detected from large distances, even beyond the heliosphere. Similar radiation can be observed from other planets featuring auroral displays, e.g. Jupiter and Saturn. A new type of AKR emission is Dot-AKR, originating from 2-3 RE radial distance, has been found to occur during substorm onsets. This is suggested to be an effect of Alfvénic wave acceleration in a pre-existing auroral cavity. In Fig. 2.6.3/1 panel a presents a lowaltitude auroral cavity associated with a stable auroral arc in the atmosphere and maintained by ion Bernstein waves. At the substorm onset (panel b), Alfvén waves arrive from the magnetosphere, causing electron acceleration (via a resonance between waves and electrons) and possibly also Dot-AKR emission in the low-altitude cavity; the Dot-AKR emission is usually short-lived and probably requires strong transient Alfvén waves. If Alfvén wave activity lasts for some time, electron acceleration causes some ions to leave the Figure 2.6.3/1: Plasma processes that Alfvén waves cause in auroral regions. resonance region as well, leading to another density cavity at higher altitudes (see panel c) found by the authors in the earlier studies. After the Alfvén wave activity has stopped, the cavity fills up on the ion time scale, so that it continues to exist for some time (panel d). The low-altitude depletion is all the time maintained by other processes that are independent of Alfvénic activity. Normal AKR is emitted all the time near the lower boundary of the cavity, although not shown. 2.6.4 Magnetospheric observations Double cusp and reconnection hypotheses Magnetic reconnection has been successful in explaining the main features of mass, energy and momentum transfers from the solar wind into the magnetosphere. A key parameter ruling the magnetic reconnection process and therefore the whole solar wind-magnetosphere coupling is the interplanetary magnetic field (IMF) orientation. For southward IMF, reconnection takes place at the low-latitude magnetopause, between the two cusps. sec2.qxd 7/11/05 5:13 PM Page 33 research activities 33 Figure 2.6.4/1: Statistics of cusp observations from Cluster. The signature of low-latitude reconnection is a strong anti-sunward convection in the cusp as well as an energy dispersion of ions (higher energies at lower latitudes). For northward IMF, on the other hand, reconnection takes place at higher latitude, poleward of one or both cusps. This drives a sunward convection in the cusp and the ion energy dispersion is then ‘reversed’ (higher energies at higher latitudes). An intermediate case appears when the IMF is dominated by its Y-component (dawnward or duskward IMF). Then, reconnection is thought to occur simultaneously at high and low latitudes. The discovery of the double cusp and the study of its consequences in the high-latitude ionosphere makes the coupling processes between the solar wind and the magnetosphere more complicated than described above. Prior to the study of the double cusp, F. Pitout and C.P. Escoubet performed a statistical study of three months of Cluster crossings of the mid-altitude (at 56 RE) cusp (Fig. 2.6.4/1). A few morphological features of the cusp have been defined and then related to the prevailing IMF. The double cusp, which is thought to occur when the IMF is dominated by its Y-component, is searched for throughout this study. The preliminary study reveals, among others, that textbook cases of cusps with nice ion dispersions do not occur that often. Instead, numerous irregular and discontinuous cusps are found, among which there are interesting cases of discontinuous cusps occurring under stable IMF conditions. The latter are also good candidates for stable double cusps, which require further studies. Banded hiss emissions in the plasmasphere The inner part of the magnetosphere contains two important regions: radiation belts that contain relativistic electrons, and a plasmasphere that contains cold plasma originating from the ionosphere. Plasmaspheric hiss (at 100-10 000 Hz) is observed throughout the Earth’s Figure 2.6.4/2: WHISPER spectrograms Cluster 1 (top) to Cluster 4 (bottom) from plasmasphere, particularly during high magnetic activity. This emission cuts off suddenly at the plasmapause, the outer boundary of the plasmasphere. Although the generation of hiss emission is not yet understood, it is believed that the decay of radiation belt electrons is significantly controlled by the hiss phenomenon. Using Cluster instrumentation (WHISPER, STAFF and WBD), an investigation into plasmaspheric hiss was initiated which established a previously unknown phenomenon, banded hiss emission (BHE) (Masson et al., 2004). It appears below the electron gyrofrequency, Fce, but above the lower hybrid resonance, from 2 kHz to 10 kHz. The waves were shown to propagate in the whistler mode. Based on the first year of Cluster observations, the following properties of the BHE waves were identified: (i) the location is strongly correlated with the position of the plasmapause; (ii) no MLT dependence was found; (iii) the spectral width is generally 1-2 kHz; (iv) the central frequency of their emission band varies from 2 kHz to 10 kHz and correlates with the Kp index. All these features suggest that BHE is in fact mid-latitude hiss (MLH). The central frequency correlation with Kp, found by this study, is a new property of MLH. It suggests either that MLH is generated in a given f/Fce range, or that there is a Kpdependent Doppler shift between the satellites and a possible moving source of the MLH. sec2.qxd 7/11/05 5:13 PM Page 34 34 Figure 2.6.4/2 shows an example of MLH as observed by WHISPER on 2001 October 7, 14:45-18:30 UT. MLH occurs at 16:25-17:04 UT, indicated by white arrows. MLH is found to intensify with altitude and with time (note that the four Cluster satellites fly in a string-ofpearls formation near perigee). 2.6.5 Examples of other associated activities within SCI-SH In addition to the analysis of Cluster data, the team is also involved in the analysis of magnetospheric data from Double Star. The Double Star TC-1 spacecraft carries an ASPOC instrument that keeps the satellite potential near zero with respect to the ambient plasma. The team, through SCI-A, contributed both hardware and expertise on ion emitter development and in-flight operations to ASPOC. The ion emitter module was improved after experience gained on the Cluster mission. After the successful launch on 29 December 2003, ASPOC is functioning very well with a very good high-voltage ignition and very stable ion current. The PI institute of the instrument is the Space Research Institute in Graz (A). Moving from the study of the Earth’s magnetosphere through the Cluster and Double Star missions, the research group is now turning its attention to the magnetosphere of Mercury. The team is involved in the challenging (owing to the very high temperature environment) development of an electric field instrument for the BepiColombo/MMO satellite. The team is responsible for the thermal analysis of the overall instrument, which is delegated to SCI-A personnel for implementation. The PI institute of the instrument is the Royal Institute of Technology in Stockholm (S). In addition, the study of ions from the surface of Mercury and their interaction with the planet’s magnetic field will be explored through the group’s involvement in the PICAM ion spectrometer on the BepiColombo MPO (Co-I C.P. Escoubet). Here, the design of the analoguedigital hybrid ASIC electronics together with the MCP detectors is the responsibility of SCI-A in support of the Co-I. Finally, the SMART-1 satellite carries the SPEDE instrument that monitors the performance of the solar electric propulsion (SEP) engine of the satellite. The Division, together with SCI-A personnel, has been involved in the design and manufacturing of the two booms as well as the testing and calibration of the overall instrument. Measurements have been obtained since early October 2003, and currently the team is working with in-flight calibration issues. The PI institute of the instrument is the Finnish Meteorological Institute in Helsinki. Such experience will be invaluable for the BeppiColombo mission to Mercury, which also will use an SEP motor. research activities References Janhunen, P. et al. (inc. Laakso, H.), 2004, Ann. Geophys. 22, 2213-2227. Masson, A. et al., 2004, Ann. Geophys. 22, 2565-2575. Sanderson, T.R., Marsden, R., Tranquille, et al., 2003, Geophys. Res. Lett. 30(19), 8036. sec2.qxd 7/11/05 5:13 PM Page 35 research activities 35 2.7 Comparative Planetology and Astrobiology Comparative planetology is an important study area in RSSD, because it is a necessary element in the preparation of ESA’s current and future planetary missions, and it maximises the scientific exploitation of these missions. Studies of the Moon, Mars, Venus, Titan and Mercury provide unique opportunities to improve our understanding of the processes and factors that have shaped our own planet. Mars Express, SMART-1 and BepiColombo have the potential for developing expertise and knowledge in comparative planetology focused on the terrestrial planets. Venus Express, to be launched in 2005, offers similar opportunities, in particularly for climatology. Huygens will provide detailed information on one of the most mysterious objects in the Solar System, Saturn’s moon Titan. 2.7.1 Mars research Geologic evolution of the Martian surface Gusev Crater is the landing site of one of the NASA Mars Exploration Rovers (MERs). During the early commissioning period of Mars Express, the HRSC took a number of images over the Gusev area. The study of this area, including the neighbouring highlands to the south and lowlands to the north, has been the subject of a stagiaire project. Data from Mars Global Surveyor, Mars Odyssey and the recent Mars Express image and altimetry data have all been used to produce a geological map and geological profiles of the region (Fig. 2.7.1/1). The basis for these geological profiles was provided by HRSC digital elevation models (DEMs) derived from the HRSC stereo images. The resolution of these DEMs is better than the available MOLA altimetry data (better than 200 m for HRSC, compared to 600 m horizontal resolution for MOLA). Geological mapping of the surface combined with geometrical analysis of the geological profiles make it possible to determine the stratigraphic sequence, including estimates of the thickness of the various units. This provides a much enhanced insight into the geological evolution of this terrain. Some of the main issues are: (1) a relative stratigraphic sequence of 16 units, including sediments and volcanic rocks; (2) mapping of tilted Noachian terrains, indicating a dynamic early history of Mars; (3) correlation of two potential sedimentary units in the Gusev crater. Figure 2.7.1/1: Geological map of the Gusev crater on Mars. The landing site of Spirit, one of the MER landers, is also shown. The map distinguishes various rock units and is based on both image data and topography data from HRSC on Mars Express. — characterisation of surface morphology and textures at high/super resolution; — characteristics of present and future landing sites. In addition, HRSC data have been used to study the evolution of the Martian surface through time and geological processes. Specific issues being addressed by HRSC Co-I B. Foing and collaborators are: HRSC has obtained new evidence for geological activity on Mars. Calderas on five major volcanoes in the Tharsis and Elysium regions have undergone repeated activation and resurfacing during the last 20% of Martian history. Caldera floors as young as 100 Ma and flank eruptions as young as 2 Ma have been found. These results confirm that the volcanic edifices are characterised by episodic phases of activity and suggest that volcanoes are potentially still active today. — role of water and volatiles; — impact craters processes; — evolution of volcanism and hydrothermal activity; HRSC images have provided convincing evidence of a current frozen body of water, with surface pack-ice, around 5°N/150°E in southern Elysium (Murray et al., sec2.qxd 7/11/05 5:13 PM Page 36 36 2005). The study of tropical to mid-latitude glaciation on Mars shows evidence of snow and ice accumulation and flow in Mars Express HRSC data (Head et al., 2005). Finally, very young volcanic and glacial activity at Hecates Tholus has been discovered in HRSC images. In preparation for future missions to Mars involving a potential lander, Mutual Impedance Probes have been built for atmospheric and surface investigations (Huygens, Philae). The measurement of the electric properties of surface and subsurface materials is an important issue for planetary missions. A prototype of a subsurface MIP has been developed, which will allow the measurement of the profiles of the electrical conductivity and permittivity along the path of a drill or mole, and generate 2-D images of the electrical properties of materials along the walls of the borehole. The environmental parameters and requirements for applications on Mars have been analysed. This will allow the investigation of otherwise invisible subsurface structures, and the detection and localisation of subsurface water deposits. Study of the upper Mars atmosphere The research team is also closely involved in the study of the Martian atmosphere. Specifically, the UV spectrometer SPICAM aboard Mars Express is performing a number of different scientific observations, including limb measurement. These observations aim at studying the airglow (natural emission) of the upper atmosphere. From such data, information can be deduced on the composition and thermal structure of the coupled neutral atmosphere/ionosphere, on both the dayside and the nightside, and on the interaction with the solar wind. SPICAM has provided the first spectra of the upper atmosphere since Mariner-9 in the 1970s. A number of limb data spectra are being analysed in detail and show emissions of O, CO, CO2+. A model of the ionosphere (Morel et al., 2004; Witasse et al., 2003) is being updated in order to model the lines and bands detected by SPICAM. 2.7.2 Lunar studies The Moon bears the scars of countless impact craters, and holds the only accessible record of the conditions in the Earth-Moon system over the past 4.5 billion years. The recent Clementine and Lunar Prospector missions provided the first views of global geochemistry. The SMART-1 mission will add the first global IR dataset and the first global measurements using X-ray fluorescence, which will map elemental Mg, olivine and pyroxenes across the surface. These are critical to understanding the Moon’s crustal evolution and origin, which is intrinsically linked to the early evolution of the Earth, as well as other geological process in the Solar System, such as volcanism, tectonics, impact cratering and volatiles. research activities The research team (B. Foing, D. Koschny, M. Almeida et al.) is therefore actively involved in SMART-1, specifically with the AMIE imaging and the D-CIXS X-ray spectrometer teams. In particular, a new technique has been developed for remote sensing determination of lunar surface composition based on AMIE data. The approach is based on spectral and composition data derived from a Lunar Soil Characterization Consortium for a few, particle-size, separates of lunar soils, mapping the abundance of TiO2 and FeO, pyroxene content, maturity degree (Is/FeO), and a characteristic size of particles (Shkuratov et al., 2003). 2.7.3 Cassini-Huygens data analysis preparation Preparations for the arrival of Huygens at Titan: Huygens radar tests The main objective of the Huygens Radar Altimeter is the determination of the Probe altitude, which is very important for an optimised operation of the payload. In order to assess the performance of the radar at high altitudes, and verify the characteristics for concurrent operation of both radars, the research team supported a series of radar tests on the ground and aboard stratospheric balloons (HASI Sicily flight June 2003, sky test; PEASMA balloon flight November 2004). The radar signal reflected by Titan’s surface contains important information about surface properties such as roughness and electrical parameters. The signal is processed via the PWA experiment, which is part of HASI. In addition to verifying the altimeter performance, the balloon campaigns provided valuable datasets for the development and test of data analysis software, which will be used for processing the radar data returned by Huygens in 2005. Preparations for the arrival of Huygens at Titan: the HASI-PWA experiment The PWA experiment will explore the atmosphere of Titan during the Probe’s descent. It will measure the electric field (AC, Schumann resonances and lightning), the atmospheric conductivity (Relaxation Probe and Mutual Impedance Probe), pressure variations (Acoustic Experiment) and signals returned from the surface of Titan by the Huygens Radar Altimeter. The preparations for the processing and analysis of Huygens data are progressing in cooperation with partner institutes in Austria (IWF), France (CETP) and Spain (IAA). Final hardware tests have been conducted in order to finalise the calibration and validate various models required for data calibration. A recent series of tests was designed to investigate the impact of the Huygens probe attitude on the measurement of electric fields (Fig. 2.7.3/1). Preparations at ESTEC include logistics, finalising the calibration sec2.qxd 7/11/05 5:13 PM Page 37 research activities 37 2.7.4 Ground-based observation of Titan winds software and preparing for the initial data analysis during the Huygens arrival event. The study of winds on Titan is a scientific objective of the Cassini/Huygens mission. Earth-based observations are attempting to provide complementary information. All Earth-based techniques employ various implementations of the Doppler measurement technique. The technique used here, however, is based on the absolute accelerometry method developed for the detection of extrasolar planets. The reflected solar spectrum from a rotating body (in Titan’s case, its atmosphere) observed by a high-resolution spectrometer was analysed. The rotating atmosphere induces a Doppler shift in the whole spectrum. Observations of Titan were performed in 2001-2002, with the UVES spectrometer mounted on the ESO VLT. However, the data reduction, analysis and interpretation using the UVES pipeline data processing tools have led to results difficult to interpret. As a result, the approach was verified by applying the method to a rotating body with no atmosphere: Io. In that case, the method consists of retrieving the surface rotation velocity, which is well known. Four observations of Io performed in early 2003 were analysed, yielding a rotation rate with an uncertainty < 2 m/s (Civeit et al., 2005). With the improved pipeline processing the method is being applied to analyse the observations of Titan, plus some recent observations of Saturn. Reconstruction of the Huygens trajectory 2.7.5 Earth comparative planetology The Huygens Project Scientist Team supported the scientific activities of the Descent Trajectory Working Group (DTWG). This group was created to ensure an orderly and efficient analysis, interpretation and delivery of the Cassini/Huygens engineering and instrument data necessary for reconstructing the the Huygens probe entry and descent trajectory. One of the major activities of the group was the implementation and testing of a numerical tool that can reconstruct the trajectory. In this context, the Project Scientist Team built a synthetic dataset of the mission in order to test the algorithm. The philosophy of the approach, the assumptions made and the limitations of the method are described in Perez-Ayucar et al. (2004). Impact cratering studies Figure 2.7.3/1: Huygens balloon model in the electric field test chamber at Padua University, Italy. Study of the upper atmosphere of Titan The upper atmosphere of Titan has been investigated by the Cassini Orbiter through two dedicated studies of the ionosphere. The first is related to the ion production due to electron impact (Lilensten et al., 2005a). The second concerns the modelling of a doubly charged ion layer that could be detected by the UVIS instrument (Lilensten et al., 2005b). This paper is the last of a series of three studies on comparative planetology devoted to the doubly-charged ions in planetary atmospheres (Mars: Witasse et al., 2003; Earth: Simon et al., submitted). Impact craters are the most common geological feature in the Solar System. All of the planets have been struck by countless asteroids, comets and meteoroids since its formation 4.6 billion years ago. Impact craters thus represent a fundamental field of research in planetary studies. The emerging view of planets as geological objects makes the search for previously unknown impact craters on Earth a fundamental element of planetary exploration. Various potential methods for the automated recognition of impact craters from remote sensing data have been considered. As a result of the study, an algorithm based on the Hough transform was selected, implemented and demonstrated to be effective in identifying known craters from sample images of the Earth, Mars and the Moon. The study also showed that the detection of new unknown impact craters requires the exploitation and fusion of data from multiple remote sensing missions and sensors, and therefore the development of more sophisticated recognition algorithms. Envisat data are being exploited in the framework of this work, to be followed by potential fieldwork of a few examples of identified structures. Of course, such an approach can also be applied to Mars craters and in particular Mars crater synthetic studies using coordinate registration by automated crater recognition. sec2.qxd 7/11/05 5:13 PM Page 38 38 Geological expedition to Pilbara terrain (Australia) The Pilbara terrain in Western Australia is one of the planet’s oldest terrains – up to 3.5 billion years old. Because of its unique record of early life and conditions on Earth, it is the focus of an international research effort organised by the NASA Institute of Astrobiology. A field expedition to the Pilbara terrain was organised in August 2004 to collect rock samples for three projects: — spectral analysis of Archean volcanic rocks as potential analogues for Martian geological units. This project is in collaboration with the Geological Survey of Western Australia, CSIRO (Australia) and Technical University of Delft, ITC (Enschede, NL); — study of the early Earth magnetic field. The behaviour of the Earth’s early magnetic field is related to the formation of the inner core. Numerical models of the geodynamo predict a weaker magnetic field at times prior to the formation of the solid inner core. So far, no record of the early geomagnetic field has been found. Granitic rocks in the Pilbara granitegreenstone terrain have been sampled for isotopic dating and paleomagnetic analysis to determine if such an early record is preserved in this terrain. This project is in collaboration with MIT and Caltech, where the measurements will be done; — sampling of units that possibly formed as a result of meteorite impacts. A 5 m-thick spherule layer was discovered in the Coongan Greenstone Belt. 2.7.6 Astrobiology Large organics in space Spectroscopy of large PAHs, including laboratory studies and comparison with the Diffuse Interstellar Bands (DIBs) have been performed by Foing and collaborators. For the first time, laboratory spectroscopy of the UV-VisNIR absorption spectra were obtained for a representative set of large PAHs that have been selected for longduration exposure experiment aboard the International Space Station and Foton/Biopan. The PAH charge distribution and DIB carriers ware also studied. Physical parameters such as density, ionisation and temperature, constrained by observed atoms and molecules, have been computed for the line of sight towards a single cloud towards HD 147889. It has been established that different wavelength regions in the DIB spectrum correspond to different charge states depending in the size distribution. The contribution of catacondensed PAHs to the strong UV 200-300 nm absorption and to the DIBs is constrained (Ruiterkamp et al., 2005). The study of DIBs’ weak unidentified interstellar absorption bands observed towards reddened stars has continued. Their carriers are believed to be large carbonaceous molecules (e.g. PAHs). The Large and research activities Small Magellanic Clouds (LMC and SMC) offer a unique opportunity to link DIB behaviour to widely varying environmental conditions (e.g. metallicity, UV radiation field and star-formation activity). To this end, the absorption spectra of reddened OB stars in the Magellanic Clouds have been observed at unprecedented high resolution (R = 100 000) and high S/N with VLT/UVES. Analysis of the spectra of the LMC and SMC targets indicates that a delicate balance must exist for DIBs to be present. Noteworthy in this respect is the 30 Doradus region in the LMC, where these special conditions seem to prevail. Of all the LMC stars observed, only the two in the 30 Dor region have detectable DIBs. This balance appears to be strongly dependent on the UV radiation field, which is represented by the shape of the extinction curve (i.e. the presence of the 2200 Å bump and the steepness of the far-UV rise). The strongest diffuse interstellar bands ever were measured using the VLT/UVES in the heavily reddened line of sight towards the high-mass X-ray binary 4U1907 +09. More than 180 DIBS could be detected in this source. The relation between the DIB carriers, and other species such as neutral hydrogen and K, could be studied. An astronomical search coupled to laboratory spectroscopy was conducted for C84: a prototype of large fullerenes. For the first time, a UV/Vis spectrum of a neutral and ionised fullerene (C84 isolated in Ne matrix) was obtained. It shows absorption bands that have been compared to the optical DIB spectrum. Finally, the ORGANICS experiment on Foton/Biopan has been prepared to study effects of UV and particle radiation on selected PAHs and fullerenes, in order to better constrain the destruction pathways of large organic molecules in interplanetary and interstellar environments. Complex organics on Mars The behaviour of organic compounds in a simulated Mars environment is under study. Viking Lander biology and molecular analysis experiments were re-analysed and possible reasons why no organic compounds could be clearly detected were identified (Ten Kate et al., 2003). The search for organic molecules and traces of life on Mars has been a major topic of planetary science for several decades. The search for extinct or extant life is the future perspective for several missions. A set of organic molecules has been selected for simulation experiments. Laboratory experiments under simulated Mars conditions are performed in order to determine what those missions should be looking for. This research has been developed as part of a Mars Express Recognised Cooperating Laboratory (RCL). sec2.qxd 7/11/05 5:13 PM Page 39 research activities The Mars simulation chamber has been used to study thin layers of glycine exposed to low ambient pressures and UV lighting conditions similar to those on Mars. Scaling times for sample alteration were determined for these Mars-like conditions. A sequence of Mars chamber studies is dealing with the Martian survival properties of ice covered by or mixed with dust. This should provide an understanding of the remnants of glacier and ice deposits during the Mars obliquity cycles, as observed by Mars Express/HRSC. References Civeit, T. et al., 2005, A&A 431, 1157. Cox, N. et al., 2004, A&A, submitted. Head, J. et al., 2005, Nature 434, 346. Lilensten, J. et al., 2005a, Icarus 174, 285. Lilensten, J. et al., 2005b, GRL 32(3). Morel, L. et al., 2004, PSS 52, 603. Murray, J. et al., 2005, Nature 434, 352. Perez-Ayucar, M. et al., 2004, ESA SP-544. Ruiterkamp, R. et al., 2005, A&A 432, 515. Shkuratov, Y. et al., 2003, Sol. Sys. Rev. 37, 251. Simon, C. et al., 2004, submitted. Ten Kate, I. et al., 2003, LPI 1, 1313. Witasse, O. et al., 2003, GRL 30, 12. 39 2.8 Minor Bodies The Minor Bodies research group explores the physical and chemical properties of some of the oldest objects in the Solar System with a view to understanding how it was formed and providing insight into the formation and evolution of extrasolar systems. Both topics are key aspects of current and future activities in the Agency’s science programme through such missions as Rosetta and Darwin. To this end, the research group uses a variety of tools, spanning the development of key instruments and observations from ground- and space-based observatories, both underpinned by a theoretical- and modellingbased programme. 2.8.1 The MIDAS instrument on the Rosetta mission The MIDAS Atomic Force Microscope onboard the Rosetta Orbiter was developed in collaboration with IWF, Graz (A). This instrument will collect, image and characterise the geometry of dust particles when in orbit around Comet 67P/Churyumov-Gerasimenko. Among the key scientific goals is the 3-D characterisation of cometary dust with a resolution of better than 10 nm and the determination of dust flux variation and statistics of particles in the size range 10 nm to 5 µm. The AFM will study the morphology of dust grains around a comet in situ rather than requiring a far more expensive sampling and return mission. After many years of development, manufacturing, integration and testing, the long-awaited successful launch of Rosetta came in March 2004. Since then, MIDAS has undergone its initial deployment and has been checked out in the majority of its operational modes. The instrument carries samples that allow a complicated but high-resolution in-flight calibration. The imaging conditions and parameters during the early commissioning phase are identical to those during the final orbit around Comet Churyumov-Gerasimenko. The data show that MIDAS is fully operational and its performance not only fulfils, but exceeds, the scientific requirements. Fig 2.8.1/1 shows an image of a calibration sample taken during flight. Repeated imaging on the same location confirms a reproducibility of the absolute dimensions of the sample in the range of a few nm. This result confirms the excellent mechanical performance of the instrument as well as the favourable imaging conditions aboard Rosetta. If all goes well with the instrument and the mission as it journeys to the comet, we shall for the first time be able to study the morphology of dust grains at the nm level from one of the early primitive bodies of the Solar System. The interpretation of flight data and further optimisation of instrument operational parameters are supported by an intensive measurement programme using the flight spare sec2.qxd 7/11/05 5:13 PM Page 40 40 research activities Figure 2.8.2/1: A part of the CN R branch of the average reduced spectrum of comet C/2000 WM1 (LINEAR) compared with the synthetic spectrum. Top panel: synthetic spectrum (thick line) contains only 12C14N. Bottom panel: the synthetic spectrum also contains 13C14N and 12C15N, which result in an almost perfect fit to the observed spectrum. Figure 2.8.1/1: The MIDAS flight instrument shortly before integration on the spacecraft. Below: the first image taken in space during Rosetta’s commissioning phase shows the cubed structure of an onboard calibration sample. The 3-D view is rendered from raw data. Solar System. From the ground, such isotopic ratios can in principle be determined by high-resolution spectroscopy (R ≥ 700 000) of the resonancefluorescence bands of certain simple molecules containing the relevant element. In the case of the 12C/13C ratio, this has been done over the past two decades for a few bright comets, whereby the observed molecules were usually CN and C2, trace gas species typically present in cometary comae. model installed in a vacuum chamber within the SCI-A laboratories. This model is used as a testbed for new inflight procedures as well as a tool for the scientific interpretation of the flight data from the comet. For this purpose, a large number of specific samples that resemble different physical and chemical properties of cometary dust were installed. Data and experience gained during future studies will be collected and inserted into a database. This includes the growing knowledge of cometary materials from other space missions. The PI-team supported by the RSSD Co-I activity should be well-prepared to face the rigours of the encounter in order to exploit and maximise the return from this novel instrument. The analysis of high-resolution spectra of comet C/1995 Q1 (Hale-Bopp) and C/2000 WM1 (LINEAR) resulted in the optical detection of 12C15N, which permitted the 14 N/15N ratio in CN to be derived for the first time. The 14 N/15N ratios were determined to be 140±35 and 140±30, respectively, which is significantly lower than the value in Earth’s atmosphere, usually referred to as the Solar System value of 272 (Arpigny et al., 2003a; b). 2.8.2 Determination of isotopic ratios in comets It should be noted that, over the past 2 years, the 12C/13C and 14N/15N isotopic ratios were determined in the CN coma of 12 comets of different dynamical histories (Jehin et al., 2004a). For all the comets studied so far, the 12 C/13C ratio is consistent with the Solar System value of 89, whereas the 14N/15N ratio is only half the Solar System value. The results for two periodic comets have been published (Jehin et al., 2004b). Isotopic ratios of the light elements in comets are important clues to the origin and early history of the Although remarkably similar values have been derived for the 14N/15N ratios in the CN coma of the different sec2.qxd 7/11/05 5:13 PM Page 41 research activities comets, this ratio is much lower than the ratio derived for HCN from sub-mm measurements in comet Hale-Bopp (323±46). HCN was generally believed to be the main parent of CN. However, the observations of Hale-Bopp indicate a discrepancy between the nitrogen isotopic ratios in CN and HCN, which would suggest that here is at least one additional, unknown parent of CN, with even higher 15N excess. Organic compounds like those found in interplanetary dust particles are good candidates (Aléon et al., 2003). These new findings are under detailed evaluation and sub-mm measurements have been initiated to retrieve the nitrogen isotopic ratio in comets from HCN. 41 vations on 11 February 2003, post-perihelion characterisation of this comet is now available, covering its evolution along the orbit between 2.29 AU and 3.22 AU. Broadband BVRI images and low-resolution long-slit spectra have been obtained for morphological, colour and compositional analysis of the coma and for studying the comet’s activity along its orbit (Fig. 2.8.3/1). Various observational techniques have been used to collect data for the analysis of long-term and short-term variability, from which conclusions on several nucleus properties can be drawn (Schulz et al., 2004a, and references therein). Water production rates from SOHO/SWAN observations 2.8.3 Characterisation of the new Rosetta target comet Post-perihelion monitoring in 2003 A new target comet was identified for the Rosetta mission after its launch to Comet 46P/Wirtanen, planned for mid-January 2003, was cancelled. As soon as 67P/Churyumov-Gerasimenko became a likely new target based on its classification and orbital parameters, extensive monitoring of this comet began to determine a number of basic properties. Starting with the first obser- Figure 2.8.3/1: Structurally enhanced broadband R images showing the evolution of the distinct features in the coma of Comet 67P/Churyumov-Gerasimenko between February and June 2003. The direction of the Sun and the comet velocity vector are indicated. MIDAS/AFM will provide the morphology of the associated dust grains when orbit about the comet is achieved in 2014. Since January 1996, the SOHO/SWAN instrument has been producing full-sky Lyman-alpha maps. The SWAN images can be used to study the hydrogen coma of comets down to a visual magnitude of ~12. After the retargeting decision of the Rosetta mission, the SWAN archive was searched for possible occurrences of 67P/Churyumov-Gerasimenko. The comet was identified in Lyman-alpha images obtained during its 1996 apparition, and five values for the production rate of neutral hydrogen were obtained. As cometary neutral hydrogen comes predominantly from photodissociation of water, SWAN observations can be used to estimate the water production rate of a comet. The observations suggest a perihelion water production rate of about Figure 2.8.3/2: Colour-coded nucleus bulk density (kg/m3) as a function of the spin axis obliquity, I, and argument Φ. Black areas: prolate ellipsoidal model nuclei cannot reproduce the observed light curve amplitude. Dots: observed water production rates are most closely reproduced. Solid-line areas: empirical change in the longitude of perihelion is reproduced. Dashed-line areas: empirical change in the longitude of the ascending node is reproduced. sec2.qxd 7/11/05 5:13 PM Page 42 42 research activities 8x1027 s–1 and a possible post perihelion increase of activity (Mäkinen, 2004a). Nucleus properties estimated from non-gravitational force modelling The nucleus size, shape, active area fraction, spin axis orientation, mass and bulk density of Comet 67P/Churyumov-Gerasimenko have been estimated using a sophisticated thermo-physical nucleus model. The model has to reproduce simultaneously the empirical nucleus light curve, water production rate versus time, and non-gravitational changes of the orbital period, longitude of perihelion, and longitude of the ascending node (per apparition). The results suggest that the spin axis argument is close to either 60° (obliquity 100-140°) or 240° (obliquity 40-90°). Hence, the nucleus semi-axes are likely to be roughly 2.5x1.9 km. The nucleus bulk density is at most 500 kg/m3 and the active area fraction is 4-11% (Fig. 2.8.3/2). If substantial deviations between observed and calculated water production rates are allowed (to account for uncertainties in the modelling and observational errors), the spin axis orientation and nucleus dimensions cannot be estimated, but a hard upper limit on the nucleus bulk density of 600 kg/m3 can be determined (Davidson & Gutiérrez, 2004). 2.8.4 Comet modelling As a part of a project to study the cometary particle environment, the research team has built a complex particle simulator capable of producing fractal aggregates through collisional coagulation, and simulating their evolution and dynamics in a cometary coma after being expelled from the nucleus (Makinen, 2004b). This self-consistent ballistic rigid-body particle colliding simulator can be used to study the physical properties of cometary particles, the particle environment of a comet, and even the dynamics of a meteor in Earth’s atmosphere. It is capable of producing fractal aggregates of icy particles modelled by hard or soft (metaball) spheres, to be used for creating test particles in future statistical studies of the cometary coma-particle interaction (Fig. 2.8.4/1). Instead of a predefined sticking probability, actual surface interactions are modelled and a method for calculating internal stresses and fragmentation of an aggregate is described. Simulations suggest that taking fragmentation into account has two major consequences: increase in the fractal dimension of particles, and a noticeable change in the mass spectrum of an ensemble. The work continued on extracting the size distribution of dust particles by using measurements of the scattered light at a number of wavelengths. The method is based on general light-scattering properties of particles with a power-law size distribution and places no limitation on particle shape or structure. A set of equations that relates Figure 2.8.4/1: A slice through an irregular body (outlined with solid grey at intersection surfaces) at 1 AU, depicting outgassing water molecule density. The Sun is to the right. five dust colours to five dust characteristics (power index of the size distribution, the smallest and largest particle sizes, scattering efficiency averaged over the size range, and albedo ratio for the smallest and largest particles) was applied to spectrophotometric observations of comet C/1995 O1 (Hale-Bopp). The calculated solution demonstrates how physical characteristics of comet dust change with the distance from the nucleus and how they vary for different dates of observations. The power of the size distribution was found to exceed values found for other comets and is quantitative evidence for the overabundance of small particles in Comet Hale-Bopp (Kolokolova et al., 2003). 2.8.5 Ground-based observations of comets Comet 81P/Wild 2 The pre-perihelion monitoring of the coma morphology of Comet 81P/Wild 2 revealed the presence of longlasting fan structures, which remained essentially unchanged for at least 3 months. The compositional coma analysis confirmed the depleted abundance of C2 with regard to CN in this comet. The results of the observations led to the prediction that distinct coma features were likely to be present at the time of the Stardust flyby (Schulz et al., 2003); such features were indeed detected by that spacecraft. Comet C/2000 WM1 (LINEAR) The gas and dust coma of comet C/2000 WM1 have been characterised from the analysis of optical imaging and long-slit spectroscopy. The gas coma showed a double jet structure in CN and C2, which has no counterparts in the sec2.qxd 7/11/05 5:13 PM Page 43 research activities 43 dust. The gas production rates, dust colour and particle distribution in the coma have been investigated (Lara et al., 2004). Near-IR observations led to the discovery of two sublimating components in the coma, which possibly originate from different kinds of organic material (Tozzi et al., 2004). 2.9 Fundamental Physics References Aléon, J. et al. (inc. Schulz, R.), 2003, Lunar and Planetary Science 34. Arpigny, C. et al. (inc. Schulz, R.), 2003a, Science 301, 1522. Arpigny, C., et al. (inc. Schulz, R.), 2003b, BAAS 35(4), 986. Davidson, B.J.R., Gutiérez, P.J., 2004, BAAS, in press. Jehin, E. et al. (inc. Schulz, R.), 2004a, presentation at 35th COSPAR. Jehin, E. et al. (inc. Schulz, R.), 2004b, ApJ 613, L161. Kolokolova, L. et al. (inc. Schulz, R.), 2003, J. Quantitative Spectroscopy & Radiative Transfer 79-80, 861. Lara, L.M. et al. (inc. Schulz, R.), 2004, A&A 422, 717. Mäkinen, J.T.T. in The New Rosetta Targets, 2004a, Kluwer, The Netherlands. Mäkinen, J.T.T., 2004b, Particle Accretion and Dissipation Simulator. I. Collisional Aggregation of Icy Particles, submitted to Icarus. Schulz, R., 2003a, Highlights of Astronomy, IAU, 13. Schulz, R., 2003b, BAAS 35(4), 970. Schulz, R., 2004, CNES Magazine No. 21. Schulz, R. et al., 2003, A&A 398, 345 Schulz, R. et al., 2004a, in The New Rosetta Targets, Kluwer, The Netherlands, 15-24. Schulz, R. et al., 2004b, A&A 422, L19-L21. Tozzi, G.P. et al. (inc. Schulz, R.), 2004, A&A 424, 325. The LISA Pathfinder spacecraft will carry the European LISA Technology Package (LTP) and a similar USprovided package (ST7). Both packages consist of two free-floating test masses, each in capacitive sensor cages (‘gravitational reference sensors’), which are the heart of the drag-free control and an essential part of the LISA mission. The purpose of both packages is to test a variety of operational modes of the gravitational reference sensors together with their associated µN-thrusters and drag-free loops, and to verify their performance and noise behaviour. Research in Fundamental Physics is concentrated on supporting the LISA Pathfinder and LISA missions, particularly in the area of high-precision phase measurements and interferometry. 2.9.1 Interferometer design for LISA Pathfinder The LTP interferometer is the diagnostic tool used to monitor the test masses in all operating modes continuously by measuring the distance between the two test masses, the position of one test mass with respect to the optical bench, the differential alignment of the two test masses (with two sets of measurements: DC and differential wavefront sensing), and the alignment of one test mass with respect to the optical bench. In the LTP, three heterodyne interferometers obtain these measurements, two to measure the distance and the alignment of the two test masses with respect to each other and with respect to the optical bench, and one interferometer to provide a reference signal (Fig. 2.9.1). 2.9.2 A phasemeter for LISA Pathfinder To evaluate the change in optical path length, precise determination of the phase of the heterodyne signal (typically a few kHz) is needed. The implementation of the phasemeter chosen for LTP is based on digitising the datastream with a sufficiently high sampling rate (about 100 kHz). It obtains the in-phase and out-of-phase components of blocks of input data with respect to a reference signal derived from the nominal heterodyne frequency. These components are then used to calculate the phase of the interferometric signal with respect to the reference signal. Data output occurs with a rate of 10 Hz. A laboratory prototype of this phasemeter (Fig. 2.9.2/1) has been employed successfully at the University of Hannover (D), with the active involvement of the RSSD reseach team, to measure the performance initially of a breadboard prototype of the LTP interferometer (Heinzel et al., 2004). The phasemeter, at that point still realised in software on a standard PC, was used during the test sec2.qxd 7/11/05 5:13 PM Page 44 44 research activities Figure 2.9.1/1: The Engineering Model of the LTP optical bench. campaign of the Optical Bench EM for LTP to demonstrate the compliance of the EM. In a later stage, a full LTP phasemeter, with 12 channels, 16-bit A/D converters, and the software implemented in an FPGA has been realised. Differential wavefront sensing As LTP will use quadrant photodiodes (QPDs) for the sensing of all the interferometric signals, it is possible to obtain information regarding the alignment of the test masses by comparing the relative phase of the heterodyne signals coming from the four different quadrants of the QPD. During the test campaign for the optical bench EM, an accuracy of better than 10 nrad/√Hz in the frequency range relevant for LTP was achieved using this technique. Figure 2.9.2/1: Schematics of the LTP phasemeter. Figure 2.9.1/2: Layout of the LTP optical bench. sec2.qxd 7/11/05 5:13 PM Page 45 research activities 45 2.9.3 Frequency stabilisation for LISA 2.10 Research Activities in SCI-A One of the most critical issues for LISA is the need for a laser that is stable enough in frequency to allow the detection of gravitational waves. All of the current strategies to achieve the required stability rely on a combination of pre-stabilisation and numerical postprocessing of the data. The Science Payloads and Advanced Concepts Office performs research focused almost exclusively on the needs of future ESA science missions, and specifically on advanced payload technologies. Such technologies are underpinned through a long-term coordinated material science and micro-electronics programme involving: A particularly promising approach for a laser frequency stabilisation is a control system in which the instantaneous laser frequency is compared to the laser frequency; a round-trip time of about 33 s. Owing to the long intrinsic delay, the ensuing control loop is nontrivial in design, and transients and the damping of the initial conditions become important issues. García et al. (2005) have successfully demonstrated the feasibility of the stabilisation scheme, replacing the 5 million km LISA arm by a 300 m delay line and the laser with a voltage-controlled crystal oscillator. They were able to demonstrate a noise suppression of about 40 dB up to the frequencies comparable to the inverse delay. The initial conditions on closing the control loop, i.e. the change of the laser frequency during one round-trip time, were predicted to be critical for the performance of the stabilisation scheme. García et al. showed that the influence of the initial conditions could be minimised by a suitable time-dependence of the control loop’s gain when closing the loop. References García, A. et al., 2005, Class. Quantum Grav. 22(10), S235-S242. Heinzel, G. et al., 2004, Class. Quantum Grav. 21(5), S581-S587. — — — — materials for advanced superconducting sensors; novel semiconductor sensor materials; materials for low-resource optics; application-specific integrated circuits (ASICs). 2.10.1 Development of superconducting cameras The superconducting sensor programme is one of the longer-term advanced sensor development programmes focusing on applications from the near-IR to the soft X-ray band. It has considerable heritage and combines basic research on the properties of novel superconducting thin films with direct and immediate applications of more traditional superconducting materials. Developments of practical sensors are aided by proof testing on the ground on astronomical telescopes, which provides RSSD and community astronomers with the latest astronomy instruments. A considerable effort by SCI-AI in the Superconducting Tunnel Junction (STJ) development programme was focused on completing the next-generation optical spectrophotometer, S-Cam3, for its first observation run in July 2004. This system is capable of measuring individual optical photon energy, position (imaging) and arrival time (to ~1 µs). The improvements of the new system over its S-Cam2 predecessor can be summarised as: — FOV increase from 4x4 arcsec to 11x9 arcsec. This has major system-level implications as well as bringing the S-Cam instrument closer to an astronomical instrument with wider applications; — optimised IR rejection filters, while extending the ‘red’ response; — increased energy resolution; — increased electronics readout speed and hence the system’s photon rate capability; — improved data-acquisition software robustness. The first objective was met by a redesign of the detector. The S-Cam3 detector is an array of 10x12 pixels, each 33x33 µm with 4 µm inter-pixel gaps. The increased pixel size corresponds to ~0.8x0.8 arcsec on the sky. The combined effect of a significant increase in pixel number and slightly larger pixel size ensures uncompromised photometry on point sources, even under poor seeing conditions, and a more accurate background subtraction. sec2.qxd 7/11/05 5:13 PM Page 46 46 research activities Figure 2.10.1/2: Comparison of the overall detection efficiency of S-Cam2 and S-Cam3. Future S-Cams are intended to develop the read response beyond 1 µm. Figure 2.10.1/1: The S-Cam3 array of 10x12 pixels each of 33x33 µm. Note the large amount of wiring required to connect yet isolate individual pixels electrically. Also, simultaneous imaging of more than one object becomes possible, which is useful when observing extremely weak objects. Fig. 2.10.1/1 shows a micrograph of the S-Cam3 array and highlights the complex photolithography involved in this technology. The layup of the detectors is identical to the S-Cam2 arrays: 100 nm Ta with 30 nm Al trapping layers on each side of a very uniform and thin oxide layer. The best arrays show 100% pixel yield: all 120 pixels are low-leakage STJs with typical leakage currents of ~30 pA. The responsivity (defined as the total collected charge in electrons per eV of incident photon energy) for the selected array is slightly increased from ~15000 e–/eV in S-Cam2 to ~18000 e–/eV in the current devices. For these kinds of detectors, the rejection of thermal-IR photons is of crucial importance. The low energy gap of Ta/Al STJs makes them sensitive to wavelengths up to ~1 mm. Since the detector is optically coupled to a 300K environment, the IR-rejection filters have very tight requirements. Simple calculations of attenuation factors in the vicinity of the peak of the 300K blackbody radiation could not, however, explain the excess in subgap current measured in S-Cam2. It was therefore concluded that we were suffering from residual very long-wavelength radiation. In order to optimise the suppression of the longer wavelengths, while simultaneously improving the throughput in the visible, the filter glasses were changed and an additional filter was added at 300mK. This, in combination with improved baffling and shielding, reduced the IR load per unit detector area by more than an order of magnitude. Figure 2.10.1/2 is a comparison of the total efficiency of S-Cam3 versus S-Cam2. These curves take into account the measured transmissions of all optical elements as well as the detector’s efficiency. The peak efficiency has increased from ~22% in S-Cam2 to ~30% in S-Cam3. The bandwidth (at 10% of maximum) has also increased from 335-690 nm to 330-745 nm. With the combined effect of reduced IR load and higher detector responsivity, we have been able to measure a photon wavelength resolving power R = 13 at 500 nm, up from R = 8 in S-Cam2. The electronic readout system for S-Cam3 was completely redesigned. It allows in situ verification of each individual pixel by means of I-V curve tracing. Furthermore, the preamplifier signals are immediately converted to the digital domain at up to 40 MHz sampling rates. A Finite Impulse Response filter is implemented for each channel in FPGAs, which can be reprogrammed ‘on the fly’. This allows an optimisation of the filter algorithm for either higher energy resolving power or higher speed. After event detection, the data stream is split in two. One is logged on a RAID system for off-line post-processing, while the other will be processed in the programmable hardware for quick-look purposes. In this way, light curves and spectra are displayed in real-time and updated every second without compromising raw data logging or running the risk of system failure due to computing or data-stream bottlenecks. Maximum count rates are > 8000 counts/s/pixel and > 500 000 counts/s over the whole array. With such a capability, astronomers now have an additional tool with which to investigate very high-speed phenomena in a wide range of objects. In order to cool the detector to its operating temperature of ~0.3K, a dewar in combination with sorption coolers was used. This dewar can contain ~12 litres of liquid helium. Contrary to S-Cam2, S-Cam3 uses a hybrid 4 He–3He sorption cooler combination. The hold time at sec2.qxd 7/11/05 5:13 PM Page 47 research activities 47 Figure 2.10.1/4: Processed S-Cam3 image of a 16th magnitude star showing the effect of differential atmospheric refraction. With its intrinsic ability to detect and measure the colour of every single photon with a time resolution of below 1 µs, a wide range of astronomical applications can be envisaged for this technology. Figure 2.10.1/3: S-Cam 3 cryostat (blue) with the four banks of preamplifier units (32 channels per bank) mounted. In the foreground are the relay optics and filter wheel. the base temperature of 285mK is in excess of 24 h. In combination with ~18 h hold time of the helium bath, this allows for uninterrupted stable operation throughout the night and convenient recycling during daytime. The complete system can be seen in Fig. 2.10.1/3. S-Cam3 saw first-light during a 7-night observation campaign at the 4.2 m William Herschel Telescope at La Palma (E) in July 2004. The instrument performed extremely reliably, with only 15 min of observation time lost due to instrument problems. The observation programme focused on the detection of temporal and spectral variability in a number of targets. Data processing and analysis is underway. Fig 2.10.1/4 shows a processed image of a point source under fairly poor seeing conditions. Using the detector’s intrinsic wavelength resolution, the effect of differential atmospheric refraction is clearly seen. Fig 2.10.1/5 is a processed image of 9x11 arcsec in which five different sources can be distinguished, including a galaxy in the lower right part of the image. The star in the upper left part is Mv = 19. Note that there is some distortion in this image because some pixels were lost through electrostatic discharge in the course of the S-Cam3 final assembly. S-Cam3 has taken the development and application of superconducting sensors further along the road to practical systems providing meaningful astronomical data. Further developments focusing around far larger fields of view (~1x1 arcmin) and closed-cycle cooling are now underway. Such developments may mean that Figure 2.10.1/5: A processed S-Cam3 image of a 9x11 arcsec field showing multiple points sources and a single extended source, in this case a galaxy. Future S-Cams will extend the field coverage to about 1 arcmin, allowing intrinsic multi-colour deep-field imaging for extragalactic studies. space-based applications in future science missions are not so far away. 2.10.2 Advanced semiconductor sensors While superconducting sensors will have serious applications in future astrophysics missions, sensors based on new semiconductor materials should also be beneficial to not only astrophysics but also planetary missions. Long-term developments in semiconductor detector research have included the production of pixellated detectors fabricated from GaAs. Previous work on monolithic diodes and small pixel arrays have shown sec2.qxd 7/11/05 5:13 PM Page 48 48 research activities Bump Dedicated ASIC Pixel p-layer Insulating I-Layer (40-400 µm) Substrate N-Layer (2 µm) X-ray Illumination Figure 2.10.2/1: The approach to bump-bonding a dedicated ASIC to a large-format GaAs array so that each pixel can be read out independent of all others. The inset shows an SnPb bump bond ~20 µm in diameter. Figure 2.10.2/3a: Left, the limiting energy resolution achievable for a range of compound semiconductors as a function of band-gap energy at 5.9 keV. For completeness, included are the superconductors on which S-Cam3 is based. Curves are given for average values of the Fano factor: 0.22 for superconductors and 0.14 for semiconductors. NBG and WBG show the regions in which the narrow band gap and wide band gap semiconductors lie. Materials science research within SCI-AT/AI is covering the majority of these materials. Figure 2.10.2/2a: The Medipix GaAs array (64x64 pixels) together with the vias for the SnPb bumpbonds (inset). unprecedented performance as X-ray spectrometers due to the focus within SCI-AT on the fabrication of extremely high-quality epitaxial GaAs material. Spectroscopic performance approaches that of conventional silicon detectors, but with important advantages of higher temperature operation (owing to its larger energy bandgap) and enhanced radiation damage tolerance. The most recent activity has centred on the production of larger arrays that can be bump-bonded to readout ASICs (Fig. 2.10.2/1). A method of thinning away the supporting semiconductor substrate to expose the detecting volume and processing the contacts to allow a low temperature bonding to the readout chip matched to the detector pixels has now been demonstrated. Figure 2.10.2/2b: An X-ray image of a sardine taken with the SCI-AT GaAs array coupled to a Medipx ASIC (top). The optical image (bottom is shown for comparison). In lieu of a spectroscopic readout ASIC that is still in development, an imaging system of the same physical dimensions has been adopted from the medical imaging community. A complete end-to-end demonstration of a representative imager system has thus been possible, not only demonstrating the necessary packing technology for future space mission applications, but also affording a significant spin-off in terms of improving existing medical imager technology – GaAs can replace Si pixel arrays with the benefit of improved spatial resolution and sec2.qxd 7/11/05 5:13 PM Page 49 research activities Figure 2.10.2/3b: Measured 241Am and 55Fe energy loss spectra in (a) 1 mm2, 500 µm-thick Si detector; (b) a 1 mm2, 40 µm-thick GaAs detector; (c) a 3.142 mm2, 2.5 mm-thick CdZnTe detector; (d) a 7 mm2, 500 µmthick HgI2 detector. These wide-bandgap semiconductors are all suitable for applications in hard X-ray and gamma-ray planetary physics and astronomy. lower patient dose through the enhanced detection sensitivity (Fig. 2.10.2/2a, b). This work is expected to continue with the transfer of the same technology to the bump-bonding of a spectroscopic readout ASIC. This will be concluded by the demonstration of simultaneous imaging and spectroscopy at X-ray wavelengths. Such a technology would then be suitable for a low-resource X-ray planetary surface mapper, that in combination with suitable optics (see Section 2.10.3) can map the surface distribution of chemical elements. Indeed, this technology development has already led the scientific community to want it to form the baseline for the X-ray imaging spectrometer on ESA’s BepiColombo mission to Mercury. In addition to this specific development in GaAs, research continues on a number of other materials suitable for hard X-ray and gamma-ray astrophysics. The study of imaging sensors based on the wide bandgap semiconductors HgI2 and TlBr are particularly promising (Fig. 2.10.2/3) for room-temperature operation in the gamma-ray regime. Finally, low-bandgap semiconductors are also now being studied for the UV, EUV and soft X-ray part of the spectrum as potential imaging photon-counting sensors for astrophysics. Here the energy resolution would be improved over Si-based sensors while the needs for very low-temperature cryogenic cooling, such as required for superconducting sensors, may be relaxed (Fig. 2.10.2/3a). 49 Figure 2.10.3/1: The improvements in the stacking and orientation of fibres used in micro-channel plate optics. On the left is the old technology with rounded edges that impede stacking. At right is the current improvement, together with a high-resolution image of a few micro-channels, each ~10 µm in width. 2.10.3 Development of advanced optics To enable future low-mass (hence lower cost) astrophysics missions, SCI-AT has been developing lightweight optics using a number of different technologies for applications at X-ray and gamma-ray wavelengths. Future developments include expanding this area of research to optical and IR wavelengths in support of the Cosmic Vision programme. As an example of the power of this type of focused research and development, consider the case of microchannel plate-based optics. Micro-channel plate glass technology has been adapted for X-ray reflecting optics, where square pore glass micro-channels efficiently reflect X-rays up to a few keV in energy. When such a glass plate is slumped to an appropriate shape, and two plates located back-to-back, an approximation to classical Wolter X-ray optics can be obtained. Recent activities have centred on improving the metrology and preparation of drawn glass fibres, together with improvements in fibre stacking. Major improvement in the quality of the micro-channels has allowed improvements in performance (Fig. 2.10.3/1). Measurements made at synchrotron facilities confirm a significant improvement in attainable resolution, to ~30 arcsec. The large open area factor guarantees a very low density of the optics, such that a geometric area of 1 m2 will weigh only 25 kg. Clearly, such low-mass optics have applications not only in astrophysics missions but also as the optical part of an imaging X-ray spectrometer for future planetary missions, such as the BepiColombo mission to Mercury. Notwithstanding this dramatic demonstration of performance, a number of future applications in astrophysics demand a much higher angular resolution in order to resolve distant populations of galaxies forming early in the Universe. For the XEUS mission, for sec2.qxd 7/11/05 5:13 PM Page 50 50 research activities (Fig. 2.10.3/3). This facilitates a mission concept for XEUS that allows a 10 m2-class telescope to be transportable to an L2 orbit. It is through these types of developments, when coupled with novel deployment techniques, that high-precision low-mass optics may have serious applications on future ESA science missions over a number of different wavelengths. This may enable more demanding scientific missions to be realised while still constraining costs. 2.10.4 Advanced instrumentation research for planetary missions Figure 2.10.3/2: An X-ray image of a point source observed through the micro-pore optics. The resolution is ~3 arcsec. Such a technology will have wide applications for future ESA astrophysics missions. Figure 2.10.3/3: The low-mass micro-pore optics with a resolution of ~3 arcsec and an area-mass density at 1 keV of 200 kg/m2 (left). At right is the full-sized high-mass XMM optics, having a resolution of ~14 arcsec and an area-mass density of 2300 kg/m2. example, a requirement (goal) of 5 (2) arcsec is necessary to avoid confusion between faint objects. Another technological solution has been developed to address this need. With a long focal length, a conical approximation to Wolter optics can be obtained with excellent resolution. Such a conical approximation is realised with silicon micropores that are fabricated by a chemomechanical ribbing of highly polished silicon wafers. The structure is in principle light and self-supporting. Prototype modules produced in the last year have been measured at synchrotron facilities (Fig. 2.10.3/2) and shown already to offer an angular resolution of ~3.5 arcsec FHWM, sufficient to meet the requirements of XEUS. The area density of this technology allows a significant area-mass density advantage over, for example, the XMM-Newton replicated optics approach The Planetary Exploration Studies Section is involved in a wide range of research and development activities for remote sensing and in situ instrumentation for planetary applications of future missions. The aim is to develop scientific instruments with reduced resource demands (power, mass, volume, number of interfaces, etc) by miniaturisation, integration and use of the most recent technologies. This approach leads to sophisticated instrument suites for smaller and less demanding science missions and enables new mission profiles at reduced costs. Breadboards of several key instruments and instrument suites are under development to demonstrate scientific performance under environmental conditions and to allow a better understanding of the operational needs of future missions and the associated scientific instrumentation. Exploitation of missions in orbit or under development, such as SMART-1, Mars Express, Venus Express, Rosetta and Huygens, is also supported to investigate Figure 2.10.4/1: Refraction and total reflection at an interface between two media with refractive indices n1 and n2 (n1 < n2). The exponential decay of the electric field in a layer close to the interface, in the case of total reflection, is indicated and the symbol of a water molecule on the surface is shown. sec2.qxd 7/11/05 5:13 PM Page 51 research activities 51 current limitations, fields for further improvements, applicability of technology development and to define further needs of future enabling key technologies. Listed below are the most important activities currently under study. These developments are performed in close cooperation with various scientific institutes, industrial partners, national agencies and several ESA departments. A summary of a few of these developments are also provided below to complement the list. Note: FM = Flight Model, LM = Laboratory Model; BB = breadboard; dev/ment = development.. Research & Development Highly Integrated Payload Suites (HIPS) Laser altimeter (surface topography from orbit) Atomic Force Laboratory, metrology and MIDAS Rover (surface science with mobility) Mole (subsurface science) Heat flow and physical properties package (for the Mole) Geochemistry package (for Rover) [alternative to LMS] Laser Mass Spectrometer (LMS) LIBS-RAMAN spectroscopy Attenuated Total Reflection Spectrometer (ATR) Luminescence surface dating (sample age determination) Melting probes (subsurface science) 3-axis fluxgate magnetometer front-end ASIC Subsurface & surface radar (topography & subsurface science) Status Target level dev/ment BB study BB FM BB LM study LM, FM EM BB BB LM BB BB study BB BB BB study BB dev/ment BB FMASIC & BB BB study Attenuated Total Reflection (ATR) Spectrometer Figure 2.10.4/2: The Nanokhod rover under development within D/TEC. The payload cab can accommodate the LMS together with a micro-camera or an alternative geochemistry package under development within SCI-AP, comprising an alphaproton-X-ray and Mossbauer spectrometer. Figure 2.10.4/3: Laboratory prototype of a packetsized mass spectrometer. The oversized power connector and lens holder would be eliminated for a flight version. The starting approach here has been to consider the detection of water sublimations on subsurface soil grains on Mars with a miniaturised spectrometer based on the Fahrenfort principle (Fig. 2.10.4/1). Initial tests with commercial equipment have led to promising results that indicate the elemental composition of the grain itself may also be derived. The goal for the instrument front-end is a diameter smaller than 3 cm, so as to be accommodated as part of the payload of the mole that isalso under development for subsurface investigations. Laser mass spectrometer (LMS) This instrument is being developed together with the University of Berne to be accommodated inside the payload cab of a microrover (Fig. 2.10.4/2). Early results Figure 2.10.4/4: LMS flight-like electronics for the second prototype spectrometer (laser control circuitry and high-voltage power supply). sec2.qxd 7/11/05 5:13 PM Page 52 52 from the first rover prototype LMS, with dimensions of a few cm, its total mass and a laser source similar to those envisaged for the flight model are very promising (Fig. 2.10.4/3). A mass resolution and transmission in good agreement with simulations have been achieved. The mass resolution is sufficient to resolve adjacent isotopes clearly when used with laboratory dataacquisition hardware. Work is ongoing to improve the hardware: final miniaturisation of the electronics and optics, and setting up a laboratory testbed for performance verification and further improvements (Fig. 2.10.4/4). 3-axis flux gate magnetometer An ASIC containing the complete front-end electronics for a 3-axis fluxgate magnetometer is under development. An integrated sigma-delta converter is used to sample the output of the three magnetometer coils. The output is passed through an integrated decimation filter unit. Up to four housekeeping data channels are supported on chip. Data output and instrument control is provided via a synchronous serial interface. All required excitation signals are also provided by the ASIC. Experience gained through the successful and completed development and application of the Particle Detector Front End (PDFE) ASIC, which is due to fly on the NASA STEREO mission within the IMPACT instrument suite, has been used to ensure that an instrument on a single chip can be developed. The development, research and verification of the magnetometer ASIC is expected to be a leading example for further integration of instrument front-ends on ASICs. MIDAS An atomic force microscope has been successfully developed into a flight model and accommodated on the Rosetta mission. Laboratory tests are beingperformed with a commercial AFM and with the spare FM to build a reference database. This experience may well lead to the design of a much lower-resource instrument for incorporation into the payload of future planetary missions based around mini-satellites. research activities sec3.qxd 7/15/05 10:01 AM Page 53 53 3. SCIENTIFIC SUPPORT ACTIVITIES IN RSSD & SCI-A 3.1 Astrophysics Missions Division 3.4 Fundamental Physics Missions Division 3.1.1 3.1.2 3.1.3 3.1.4 3.1.5 3.1.6 3.1.7 3.1.8 3.1.9 3.1.10 3.1.11 3.1.12 3.1.13 Introduction and overview Herschel Planck Eddington COROT Gaia JWST Astro-E2 Darwin XEUS Lobster-ISS ROSITA EUSO 3.4.1 3.4.2 3.4.3 3.4.4 3.4.5 Introduction and overview LISA Pathfinder LISA ACES Microscope 3.5 Space Telescope Operations Division 3.5.1 3.5.2 3.5.3 3.5.4 3.5.5 HST observation programme Special HST programmes Instrument status The European Coordination Facility HST operational status 3.2 Solar and Solar-Terrestrial Missions Division 3.6 3.2.1 3.2.2 3.2.3 3.2.4 3.2.5 3.2.6 3.2.7 Introduction and overview Ulysses SOHO Cluster Double Star Solar Orbiter Solar-B Science Operations and Data Systems Division 3.3 Planetary Missions Division 3.6.1 3.6.2 3.6.3 3.6.4 3.6.5 3.6.6 3.6.7 3.6.8 Introduction and overview ISO XMM-Newton Integral Astro-F Herschel Science Centre development Information technology support activities Archive and Virtual Observatory activities 3.3.1 3.3.2 3.3.3 3.3.4 3.3.5 3.3.6 3.3.7 Introduction and overview Cassini/Huygens Rosetta Mars Express Venus Express BepiColombo SMART-1 3.7 Science Payload and Advanced Concepts Office 3.7.1 3.7.2 3.7.3 3.7.4 3.7.5 Science Payload Instrument Section (SCI-AI) Science Missions Section (SCI-AM) Planetary Exploration Studies Section (SCI-AP) Advanced Technology Section (SCI-AT) Darwin special project group sec3.qxd 7/15/05 10:01 AM Page 55 scientific support activities 55 Section 3 addresses the contributions of RSSD and SCI-A staff to the mission-related activities of the Department and Office. These encompass ESA’s science missions in their orbital and post-operations phases, the approved missions under or awaiting development, and missions under study. ‘Europeanised’ missions led by a national agency and potential International Space Station (ISS) payload elements are also included. The chapter is structured by Division, reflecting the RSSD organisation at the end of the reporting period (see Table 1). As stated in Section 1, RSSD has four Mission Divisions (Sections 3.1-3.4) and two Operations Divisions (Sections 3.5 and 3.6). The responsibilities of the Science Payload and Advanced Concepts Office, which are independent of RSSD although closely associated, are summarised in Section 3.7. For astronomy missions (excluding HST), the Astrophysics Missions Division has responsibility for Project and Study Scientist support until in-orbit commissioning. Responsibility for the development and execution of science operations and, after completion of the in-orbit commissioning phase, for the mission management rests with the Science Operations and Data Systems Division. Responsibility for mission management of Solar, Solar-Terrestrial and Planetary Missions during operational phases remains, however, with the respective Mission Division. The Space Telescope Operations Division hosts the ESA staff supporting the Hubble Space Telescope Science Institute (STScI) in Baltimore (US) and the European Coordinating Facility (ST-ECF) in Garching (D). For the sake of brevity, the instruments, Principal Investigators, mission or interdisciplinary scientists, science team members etc. of the missions described are not tabulated here. Such information may be found in ESA’s Report to COSPAR, the most recent being ESA SP-1276 (July 2004), produced by the RSSD Project Scientists, and in the relevant Web pages (the addresses are included here as footnotes with each mission description). Table 2: Research and Scientific Support Department 2004 – Projects and Studies. Division Astrophysics Missions Missions in Operation or Post-Operation/ Archive Phase Solar & Terrestrial Missions Planetary Missions Ulysses SOHO Cluster Double Star Cassini/ Huygens Rosetta Mars Express SMART-1 Venus Express BepiColombo Missions in or awaiting development Herschel Planck Eddington JWST Gaia COROT Solar Orbiter Mission and ISS Payload Studies Darwin XEUS ISS* ILWS Solar-B * Lobster-ISS, EUSO, ROSITA Fundamental Physics LISA Microscope LISA Pathfinder ACES Space Telescope Operations Science Ops. & Data Systems HST ISO XMM -Newton Integral Astro-F Herschel science ops. sec3.qxd 7/15/05 10:01 AM Page 56 56 3.1 scientific support activities Astrophysics Missions Division Madrid, Spain, the location of the Herschel Science Centre during operations. 3.1.1 Introduction and overview The past 2 years brought their share of good and bad news. On the sour side, the financial situation of the Science Programme forced the cancellation of the Eddington mission by the SPC at the end of 2003. This was particularly sad given the strong scientific case of Eddington and its wide support in the scientific community. The latter is illustrated by the highly successful Eddington workshop organised by the Division in April 2003 in Palermo. The excellence of Eddington was also reaffirmed in 2004 by the SPC, who recommended that it should be the first mission to implement if additional money could be found. The Columbia Shuttle accident in 2003 and the US decision to terminate the ISS and Shuttle programmes soon after 2010 were serious drawbacks to various projects under study in the Division. The Division’s Study Scientist, supported by the D/HME Study Manager, expended considerable effort in investigating alternative launch scenarios for the EUSO high-energy cosmic-ray payload. However, mostly due to its large size and mass, it soon became clear that there would be no credible transportation system to lift EUSO into orbit and install it on the ISS. Irrespective of these programmatic uncertainties, the AWG and FPAG jointly re-examined the science case of EUSO during Spring 2004. Both working groups confirmed that the scientific potential of EUSO was excellent but not among their top priorities, and therefore did not recommend its continuation into Phase-B. The early retirement of the ISS was also potentially bad news for XEUS because the original mission profile foresaw assembling the mirrors in orbit at the Station. Fortunately, a breakthrough in the development of light X-ray mirror technology by SCI-A meant that the ISS is no longer needed and that a 10 m2 mirror spacecraft can be injected directly into an L2 orbit by an Ariane-5-type launcher at a much reduced cost. The gradual build-up of the Herschel Science Centre (HSC) operations team continued throughout the period. Members of the team spent extensive periods at the PI institutes, working together with the PI teams to prepare for the scientific operations of Herschel, and for the calibration of its instruments. They were deeply involved in the Instrument Level Tests (ILTs) successfully carried out in Autumn 2004. The Herschel Common Science System (development led by RSSD) was used to support the ILTs and archive the test data. This rather hectic period ended happily with the delivery of the instrument cryo-qualification models to ESA in late 2004. The HSC team is now busy preparing the first call for observing proposals, which will be issued in 2006. In April 2005, the team will relocate to ESAC near With five staff in place, the small team in the Planck Science Office is now complete. The development is well under way by RSSD of the software tool needed to evaluate the quality and completeness of the survey data and replan Planck operations if necessary. The publication of the first WMAP results suggest that the detection of the so-called CMB polarisation B mode by Planck is a real possibility, thereby enhancing the scientific case for the mission even further. RSSD activities in support of Gaia have also picked up momentum. Most prominent is the development, under RSSD responsibility, of a prototype data-analysis system. This Gaia Data Access & Analysis Study (GDAAS) is intended to demonstrate the feasibility of reducing the 1000 TB expected from the 5-year mission and of iteratively extracting the positions and proper motions of ~1 billion sources. A milestone was achieved in late 2004, with the processing of 18 months of simulated data and the successful recovery of 200 000 stars. RSSD activities in support of JWST have also gained significant momentum over the last 2 years, as the project transitioned from its definition phase into implementation. In late 2003, one new staff member was added to the Division to assist the JWST Project Scientist. Both have been busy defining the scientific capabilities and detailed technical specification of NIRSpec, an instrument that is being developed and financed by ESA. They prepared the JWST Science Management Plan, which was subsequently approved by the SPC. The NIRSpec Instrument Science Team was later appointed, to provide scientific guidance to the Project Scientist. 3.1.2 Herschel The Herschel Space Observatory is a multi-user observatory-type mission targeting the 57-670 µm range in the far-IR and sub-mm, providing observation opportunities for the entire astronomical community. Herschel is scheduled for launch in mid-2007. Herschel is designed to address the ‘cool’ Universe; it has the potential of discovering the earliest epoch protogalaxies, revealing the cosmologically evolving AGNstarburst symbiosis, and unravelling the mechanisms involved in the formation of stars and planetary system bodies. A major strength of Herschel is its photometric mapping capability for performing unbiased surveys related to galaxy and star formation. Redshifted ultraluminous IRAS galaxies (with SEDs peaking in the 50100 µm range in their rest frames), as well as class 0 proto-stars and pre-stellar object SEDs, have their maximum emission in the Herschel prime band. Herschel http://www.rssd.esa.int/herschel/ sec3.qxd 7/15/05 10:01 AM Page 57 scientific support activities 57 shared with Planck. It will operate from the vicinity of L2, which is situated 1.5 million km away from the Earth in the anti-sunward direction. It offers a stable thermal environment with good sky visibility. Commissioning and performance verification will take place en route to L2. Once these crucial mission phases have been accomplished, Herschel will enter routine science operations for a minimum of 3 years. The scientific operations of Herschel will be conducted in a novel decentralised manner. The operational ground segment comprises six elements: — the Herschel Science Centre (HSC), provided by ESA; — three dedicated Instrument Control Centres (ICCs), one for each instrument, provided by their PIs; — the Mission Operations Centre (MOC), provided by ESA; — the NASA Herschel Science Centre (NHSC) provided by NASA. The HSC acts as the interface to the science community and outside world in general, supported by NHSC for the US science community. The HSC/NHSC provides information and user support related to the entire lifecycle of an observation, from calls for observing time, the proposing procedure, proposal tracking, data access and data processing, as well as general and specific information about using Herschel and its instruments. Figure 3.1.2/1: An artist’s view of the Herschel satellite as developed by Alcatel. is also well equipped to perform spectroscopic follow-up observations and further characterise interesting individual objects. Herschel’s telescope is passively cooled (to maximise size), while the three focal-plane instruments are housed inside a superfluid helium cryostat, on top of which the telescope is mounted. The instruments are provided by consortia led by PIs who get guaranteed observing time in return. The Photodetector Array Camera and Spectrometer (PACS) is a camera and low- to mediumresolution spectrometer for wavelengths up to 210 µm. The Spectral and Photometric Imaging Receiver (SPIRE) is a camera and low- to medium-resolution spectrometer for wavelengths longer than 200 µm. The Heterodyne Instrument for the Far-Infrared’ (HIFI) instrument is a heterodyne spectrometer. It offers very high velocity resolution for a single pixel on the sky. Herschel (Fig. 3.1.2/1) will be launched on an Ariane-5 RSSD is responsible for building the science groundsegment infrastructure for performing these tasks, together with the ICCs. One single system that evolves over time, rather than having separate systems for different mission phases, is being built. The initial version of this system has been delivered to the instrument teams and was successfully used to support the instrument-level tests during Autumn 2004. The observation planning subsystem is based on the NASA Spot tool used by Spitzer. In this way, not only is the effort that went into building Spot reused, but previous Spitzer users will immediately feel at home, increasing their scientific productivity. SCI-SA personnel are deeply involved in providing scientific guidance and supervision to the HSC software developers and performing the usual user acceptance tests. In the course of 2004, SCI-SA personnel in the HSC spent a large amount of time collocated at the PI institutes together with the instrument teams, first preparing and later executing the ILTs. In this way, they not only provided useful support to the PI teams, but they also acquired first-hand experience with the Herschel instruments. The HSC SCI-SA scientists have also been busy preparing or upgrading the large amount of documentation required for the scientific operations of Herschel, in particular concerning the observation scheduling, the calibration of the observatory and support to the scientific community. sec3.qxd 7/15/05 10:01 AM Page 58 58 scientific support activities In order to promote Herschel awareness in the scientific community, SCI-SA personnel have also been busy delivering talks and organising conferences related to Herschel science. In 2004 alone, there have been: Telescope Instruments — a special session on Herschel at American Astronomical Society Meeting 204 in Denver, USA on 3 June 2004; — the Beyond Spitzer and Herschel conference in Pasadena, USA on 8 June 2004; — several Herschel presentations at the SPIE conference on Astronomical Telescopes and Instrumentation in Glasgow, UK on 21 June 2004; — The Dusty and Molecular Universe: A Prelude to Herschel and ALMA conference in Paris on 27 October 2004; — a workshop dedicated to the calibration of Herschel in Leiden, NL on 1-3 December 2004. Shields Solar array Service Module Interface to Ariane Figure 3.1.3/1: The current configuration of the Planck satellite, as developed by Alcatel Space (F). On request from the Astronomy Working Group chairman, the Project Scientist also presented the status of Herschel to the AWG twice during the reporting period. At the time of writing, all SCI-SA personnel in the HSC are in the process of relocating to the European Space Astronomy Centre (ESAC) near Madrid (E), from where Herschel science operations will be conducted. 3.1.2 Planck In late 1992, the COBE team announced the detection of intrinsic temperature fluctuations in the Cosmic Background Radiation Field (CBRF), observed on the sky at angular scales larger than ~10°, and at a brightness level ∆T/T ~ 10–5. In February 2003, the WMAP team announced results on scales of about 15 arcmin with a similar sensitivity (see http://lambda.gsfc.nasa.gov for detailed descriptions of both COBE and WMAP). These fluctuations have been interpreted as due to differential gravitational redshift of photons scattered out of an inhomogeneously dense medium. They thus map the spectrum of density fluctuations in the Universe at a very early epoch. This long-sought result established the Inflationary Big Bang model of the origin and evolution of the Universe as the theoretical paradigm. However, in spite of the importance of the COBE and WMAP measurements, many fundamental cosmological questions remain open. Building on the pioneering work of COBE and WMAP, the main objective of the Planck mission is to map the fluctuations of the CBRF with an accuracy that is set by fundamental astrophysical limits, allowing us to address these fundamental questions. Planck was selected in late 1996 as the third Medium mission (M3) of ESA’s Horizon 2000 Scientific Programme, and is now part of its ‘Cosmic Vision’ Programme. The observational goal is to mount a single http://www.rssd.esa.int/planck/ space-based experiment to survey the whole sky with an angular resolution as high as 5 arcmin, a sensitivity approaching ∆T/T ~ 10–6, and covering a frequency range wide enough to measure and remove all possible foreground sources of emission. The main scientific result of the mission will be an all-sky map of the CBRF fluctuations and their polarisation. In addition, the sky survey will be used to study in detail the very sources of emission that ‘contaminate’ the cosmological signal, and will result in a wealth of information on the dust and gas in both our Galaxy and extragalactic sources. The Planck payload consists of a 1.5 m-diameter offset telescope, with a focal plane shared by clusters of detectors in nine frequency bands covering 30-900 GHz. The three lowest bands (up to ~70 GHz) are covered by HEMT-based receivers actively cooled to ~20 Kby an H2 sorption cooler. The higher frequency bands are handled by arrays of bolometers cooled to ~100mK; the H2 sorption cooler provides pre-cooling for a JouleThomson 4K stage, to which a dilution refrigerator is coupled. Since 2002, the instrument development has intensified. The qualification models have been largely manufactured and are now undergoing test. The first delivery to ESA was made in late November 2004, for integration into a full qualification satellite. This model will be tested in early 2005 in a specially designed cryochamber at the Centre Spatial de Liege (B). The flight models are under manufacture and will be delivered to ESA in mid-2005. After long and complex testing, the satellite will be launched from Kourou in mid-2007. At RSSD, activity in the past 2 years has concentrated on the build-up of the Planck Science Office (PSO), which sec3.qxd 7/15/05 10:01 AM Page 59 scientific support activities is in charge of overall scientific coordination, survey planning, archiving of the final data products and their distribution to the community. Support scientists and engineers have recently joined the group, which will move in late 2006 to its final location at ESAC. Many new documents have been written by PSO staff during the reporting period, among which the Calibration Requirements document, the Planck Science Operations plan and the Calibration and Performance Verification Phase Science Operations Plan. PSO scientists have also defined the baseline Planck scanning strategy as well as the requirements on the Planck Survey Planning and Performance evaluation Tool, and they continue to provide scientific guidance and supervision to its software developers. As for Herschel, the PSO scientists have spent long periods at the HFI and LFI institutes to support the ILTs. The cancellation of the LFI 100 GHz channel by ASI in 2002 was a severe blow to the Planck scientific capability because it removed the possibility to measure the CMB polarisation at this critical frequency, where contamination by foreground sources is minimal. The Project Scientist successfully sought a resolution from the AWG stressing the scientific importance of 100 GHz polarisation measurements. This resolution helped the HFI PI to convince NASA to provide the extra funds required to finance the development by JPL of polarisation-sensitive bolometers at this critical frequency. The Project Scientist, assisted by the Planck Science Team, has updated the scientific case for the Planck mission. The revised document, which takes into account the exciting results obtained by WMAP, will be released in mid-2005. Far from weakening the case for Planck, the WMAP data actually enhance it. In particular, the tentative detection of a very early re-ionisation epoch makes it much more likely that Planck will be able to detect the so-called polarised B-mode signal of the CMB that carries information about primordial gravitational waves generated during the inflation era. The Project Scientist also updated the Science Management Plan, the highest-level document governing the implementation of the Planck mission. The revised document was approved by the SPC in early 2004. The most important modification is the introduction of an Early Release Compact Source Catalogue (ERCSC), to be published 9 months after the completion of the first all-sky survey. The idea behind the ERCSC is to allow follow-up pointed observations with Herschel of the many compact millimetric sources that Planck will discover, including several hundreds clusters of galaxy. SCI-SA personnel have also organised several conferences and workshops to promote awareness of the Planck mission in the scientific community, including the Second Planck Symposium Setting the Scene, held in Orsay (F) in January 2004 and attended by more than 200 scientists. 59 3.1.4 Eddington The Eddington mission has two main scientific goals: — the detection of habitable planets orbiting other stars, and the determination of their frequency of occurrence and characteristics in different environments; — the understanding of the formation and evolution of stars across a wide range of key stellar characteristics (age, chemical composition, mass). While planets will be detected by looking for the small but measurable decrease in a star’s light caused by a planet’s transit, stellar structure and evolution science will make use of asteroseismic techniques. These will study stellar oscillations, as has been done with the Sun for a number of years. Both techniques require long-term very high-accuracy photometric time series (which can be obtained only from space) and thus can naturally be carried out by the same payload. The original Eddington proposal, submitted in response to the 2000 call for the F2/F3 missions, was based on a monolithic 1.2 m-diameter telescope with a large-area CCD mosaic. In May 2002, Eddington was approved as an element of the Science Programme by the SPC, with a 2009 launch date. Two parallel industrial definition studies were conducted, with Astrium Germany and Alcatel as prime contractors. These involved the complete space segment, including the payload, which is baselined to be ESA-procured. Both contractors converged to a similar payload design, involving three identical, parallel telescopes with a total collecting area of ~0.7 m2 and a six-CCD focal plane. Each telescope has a different filter, so that the resulting light curves offer colour information (a unique characteristic of Eddington). In parallel, a development activity carried out with E2V as prime contractor resulted in the development of the CCD chips for the Eddington focal plane, with the first CCD chips produced and qualified. These are based on an existing design but are produced in a large, custom format tailored to the Eddington focal plane. Organised by RSSD, the second Eddington workshop took place in Palermo (I) in April 2003, attracting more than 150 scientists. The new instrumental configuration was presented to the community, and significant progress was made in the selection of the candidate fields for the 3-years planet-finding observation. This resulted in the selection of the Lacerta field announced a few months later. Later in 2003, an AO for the Eddington Science Team was run, and resulted in the selection by AWG of eight scientists. Unfortunately, at the end of 2003 the financial situation of the Science Programme required deep cuts in the programme. Notwithstanding the high scientific rating http://www.rssd.esa.int/eddington sec3.qxd 7/15/05 10:01 AM Page 60 60 scientific support activities given to it by the ESA advisory structure, it was decided to remove Eddington from the programme, and to stop all development activities. At a meeting in 2004, the SPC reaffirmed the scientific interest of Eddington, and recommended that, should fresh resources become available to the Science Programme, Eddington would be the first mission to be implemented. 3.1.5 COROT COROT is a CNES-led mission for high-accuracy photometry, with both asteroseismology and extrasolar planet-finding among its science goals. With its 27 cmdiameter telescope and 2.8x2.8° FOV, COROT will concentrate on a limited number of relatively bright targets, and will be the first mission to perform a spacebased search for exoplanets with the transit method. In return for its contribution to the telescope optics and to the payload test and integration, the ESA Science Programme has negotiated data rights for scientists based in ESA member countries. To this effect, an AO was issued in 2002, which drew a large response from the European astronomical community, and which has resulted in the selection of a number of teams that have since then become significantly involved in the development of the mission. As a member of the COROT steering committee, the SCI-SA Study Scientist oversees the scientific aspects of the project, in particular the definition of the observing programme. His role is also to protect the scientific interests of the European teams involved in COROT. COROT is on track for launch in the third quarter of 2006. 3.1.6 Gaia Since June 2002, Gaia has been a confirmed mission within the ESA Cosmic Vision 2020 science programme, with a target launch date of mid-2011. Gaia will build on the observational principles of Hipparcos to measure detailed properties of the brightest 1 billion stars. Astrometric accuracies of 10 microarcsec at 15th magnitude should lead to 20 million stars measured with distance accuracies of better than 1%, and more than 100 million better than 5%. Tangential velocities will be measured astrometrically at better than 1 km/s for about 100 million stars, while the dedicated radial velocity spectrometer will gather radial velocities to 1-10 km/s to 16-17 magnitudes, depending on spectral type. Gaia will provide multi-colour (in 11 medium and 5 broad bands), multi-epoch (of order 100 epochs over 5 years) photometry for each object to 20th magnitude, with great care being invested in devising the photometric bands to maximise their astrophysical diagnostic power. Scientific http://sci.esa.int/corot Figure 3.1.6/1: Artist’s impression of the Gaia satellite. preparations for the mission involve the participation of some 15 working groups, taking responsibility for (amongst other aspects) the accuracy modelling, the radial velocity instrument optimisation, preparation of simulated data, and the development of a data processing framework to handle the complex and large (of order 1 Petabyte) Gaia data set. The status of the satellite and payload was presented to ESA and the Gaia science team at the mid-term presentations of the definition phase, held in September 2004 at ESTEC. The two industrial teams, Alenia/Alcatel and EADS-Astrium, separately presented the status of their detailed studies into all aspects of the Gaia satellite. These definition studies will run until mid-2005. Technical prototypes of many parts of the Gaia satellite are now under development, including the silicon carbide primary mirror, and engineering models of the astrometric focal plane with flight-representative CCDs. The final catalogues resulting from the Gaia mission are not expected to become available until at least 2-3 years after the end of mission operations, i.e. in about 2018 according to current planning. However, early release catalogues of astrometry and photometry are foreseen from early on in the mission phase. http://www.rssd.esa.int/gaia sec3.qxd 7/15/05 10:01 AM Page 61 scientific support activities The Project Scientist interfaces with the ESA Gaia Project Team, chairs the Gaia Science Team, which takes overall responsibility for all aspects of the scientific development of the mission, including coordination of the scientific working groups, and leads a small team in ESTEC supporting the community in developing plans for the analysis of the huge quantity of data that will result from the mission. At the science team level, this involves monitoring and contributing to the satellite and payload design through analysis and independent modelling, and directing and coordinating the work of the 14 scientific working groups. These cover payloadrelated aspects (such as accuracy modelling, on-board detection, photometric system instrument definition, radial velocity instrument definition); in-depth studies of specific classes of objects that present particular problems during the observations or data analysis phase (such as binary stars, double stars, Solar System objects, and reference frame definition), and aspects related to the data analysis (database design, prototype reduction system development, Grid-related studies and algorithm coordination). Altogether, some 250 member-state scientists are participating in these Gaia activities. The RSSD Project Scientist support team, under direction of the Project Scientist, supports the scientific community in this coordination effort, and takes a lead in the accuracy analysis, parameter database definition, CCD performance and calibration, telemetry definition and coordination of the data analysis prototype. The status of the scientific contributions and preparations for the Gaia mission were presented at The Three Dimensional Universe with Gaia, a major symposium held at the Observatoire de Paris, Section de Meudon (F), during 4-7 October 2004, and attended by 240 participants. Details at http://www.rssd.esa.int/Gaia include up-todate news, meetings of the working groups, information sheets, presentation material, and outreach features. 61 perpetual shadow by means of a large deployable sunshade. Further cooling of the mid-IR instrument is achieved by a dedicated solid-hydrogen cryostat. ESA’s participation in the mission was formally approved by the SPC in October 2000, and consists of four components: — provision of NIRSpec, the Near-IR Multi-Object Spectrograph covering 1-5 µm; — provision of 50% of MIRI, the Mid-IR combined Camera/Spectrograph covering 5-28 µm (through special funding from the ESA member states); — provision of the Ariane-5 launcher that will carry the observatory to L2; — contributions to JWST operations. In return for its contributions, ESA will gain a ~15% partnership in JWST and secure for astronomers from its member states full access to the JWST observatory on identical terms to those enjoyed today on HST: they will have representation on all advisory bodies of the project and will win observing time on JWST through a joint peer-review process, backed by a guarantee of a minimum ESA share of 15%. Over the reporting period, the JWST observatory and its instruments successfully transitioned from the definition phase to the implementation phase. Following the NASA selection of Northrop-Grumman Space Technologies as the US Prime Contractor, the observatory underwent an extended ‘re-plan’ exercise, the outcome of which resulted in the present 16-element 6.55 m-diameter telescope design and 4-instrument payload suite (NIRCam, NIRSpec, MIRI and FGS-TF). On the European side, the highlights and major achievements of the period included: NASA, ESA and CSA have, since 1996, collaborated on the successor to the Hubble Space Telescope, the James Webb Space Telescope (JWST). JWST is scheduled to launch in 2011 and consists of a passively cooled, 6.55 m-diameter telescope, optimised for diffractionlimited performance at near-IR (1-5 µm) and mid-IR (528 µm) wavelengths. — final approval of the inter-agency agreement governing the European consortium that will provide the Optics Module of MIRI; — successful completion of the MIRI System Requirements Review; — initiation of the MIRI PDR; — selection of EADS/Astrium GmbH as the Prime Contractor for NIRSpec; — initiation of the NIRSpec PDR; — selection of the external members of the NIRSpec Instrument Science Team; — approval of the ESA JWST Science Management Plan. The JWST telescope proper and its three instruments are to be cooled in bulk to < 50K, a temperature determined by the operating temperature of the HgCdTe detector arrays employed by the near-IR instruments. Cooling is to be attained passively by placing the observatory at L2 and keeping the telescope and its instrumentation in During 2003 and 2004, ESA’s participation in JWST was supported by RSSD through the ESA Project Scientist, joined by the Deputy Project Scientist starting in late 2003. Like the Faint Object Camera on HST before it, the NIRSpec instrument is being built by European industry to ESA’s specifications and under ESA project 3.1.7 JWST http://sci.esa.int/jwst sec3.qxd 7/15/05 10:01 AM Page 62 62 scientific support activities leadership. Hence, considerable effort by RSSD staff went into defining the capabilities and detailed technical specifications of NIRSpec. These specifications served as a basis for the contractual negotiations with industry. The JWST Project Scientist proposed a list of members for the NIRSpec Instrument Science Team (IST) and got it approved by the AWG at its meeting in May 2004. Through an AO, he later recruited the IST whose main role is to provide scientific guidance to the project. The Project Scientist also drafted the JWST Science Management Plan, which was approved by the SPC in February 2004. He also obtained a recommendation from the AWG for the addition of an Integral Field Unit to NIRSpec, which considerably enhances the scientific return of the instrument and provide a back-up in case of failure of the Micro Shutter Array. 3.1.8 Astro-E2 Astro-E2 will be Japan’s fifth X-ray astronomy satellite. The mission is being developed at the Institute of Space and Astronautical Sciences, which is now part of the Japan Aerospace Exploration Agency (JAXA), together with a number of US and Japanese institutes. The planned launch date is 2005. Astro-E2 will cover the energy range 0.4-700 keV with capabilities highly complementary to those of XMM-Newton and Integral. Following an interval when the data belong to the Astro-E2 Science Working Group, a Guest Investigator Programme will begin. JAXA has kindly offered to allocate part of the Japanese time to proposals led by European astronomers. RSSD coordinated this participation and an ESA AO was prepared. Following its release, ESA established a Time Allocation Committee to review the received proposals; the highest ranking have been forwarded to JAXA for inclusion in the Japanese part of the observing programme. 3.1.9 Darwin The Darwin mission and its potential precursor experiment GENIE (Ground-based European Nulling Interferometer Experiment) have continued development. Darwin is ESA’s mission to search for and study Earth-like planets orbiting nearby (25 pc) stars. It relies on the technology of nulling or destructive interferometry, where the appropriate phase-delays are applied to the beams from telescopes separated by many tens or hundreds of metres, thereby accomplishing destructive interference along the optical axis. This extinguishes the light from the star – which is 10 orders of magnitudes brighter than an Earth-like planet – while enhancing the light from the planet. Darwin is now projected to consist of three 3 m-class telescopes based on the Herschel telescope, each on a separate spacecraft, with a beam combiner and detector assembly on a separate satellite. Two Soyuz-Fregats will launch the four spacecraft to L2. http://www.rssd.esa.int/index.php?project=ASTROE2 Mid-IR spectroscopic observations will be able to detect and measure ozone, carbon monoxide, water and methane absorption lines, which together constitute the best possible tracers of biological activities. Since Darwin relies on the new technology of nulling interferometry, ESA and ESO are jointly studying the potential GENIE precursor instrument. This is a nulling interferometer, using the infrastructure at VLTI, ESO’s interferometer at Paranal in Chile. This instrument is planned to achieve first-light some time after 2008, and will study the Darwin target stars in detail in order to determine the dust level in the exosystems, as well as attempt spectroscopic observations of a number of the known ‘hot Jupiter’ exoplanets. In late 2003, both the GENIE Science Team and the Terrestrial Exo-Planet Science Advisory teams were appointed via a standard AO. Their role is to provide scientific advice to ESA and the Study Scientist for the definition, implementation and operation of the GENIE and Darwin projects. The two industrial GENIE Phase-A studies are progressing satisfactorily. The Study Scientist is closely involved in the on-going large R&D programme that is designed to develop the challenging new technologies required for Darwin. 3.1.10 XEUS XEUS (X-ray Evolving Universe Spectroscopy) is the potential successor to XMM-Newton. The goals of XEUS are to detect massive black holes in the earliest AGN and estimate their mass, spin and redshift through Fe line and continuum variability studies, to study the formation of the first gravitationally bound, dark matterdominated groups of galaxies and trace their evolution into today’s massive clusters, to study the evolution of metal synthesis to the present epoch using observations of hot intra-cluster gas and to characterise the mass, temperature and density of the intergalactic medium using absorption line spectroscopy. The original intention was to launch two separate detector and mirror spacecraft into low-Earth orbit with a mirror area of 6 m2. The two satellites would fly in formation, separated by the 50 m focal length of the optics. The mirror area would be then expanded to 30 m2 by the addition of further mirror segments, delivered to the ISS by the Shuttle. With the early retirement of the Shuttle resulting from the Columbia tragedy, it became apparent that this approach was no longer realistic. Instead, a revised mission concept is being examined. This consists of direct injection of separate spacecraft to L2 by an Ariane-5 or similar, and a mirror area of around 10 m2 with a spatial resolution of 2-5 arcsec. XEUS will use SCI-A’s new high-precision micro-pore optics, which provide higher performance and lower mass than the nickel replication used for XMM-Newton. RSSD has http://sci.esa.int/darwin http://www.rssd.esa.int/XEUS sec3.qxd 7/15/05 10:01 AM Page 63 scientific support activities 63 been closely involved in ensuring that the revised mission scenario fulfils the scientific goals of the mission, defining a possible payload, coordinating study activities with the Japanese partners, and holding discussions with other potential partners. 3.1.11 Lobster-ISS Lobster-ISS ESA is a sensitive all-sky monitor under study as a potential external payload on the ISS. LobsterISS will use a novel form of wide-FOV micro-channel plate X-ray optics, and will be the first true imaging X-ray all-sky monitor. Lobster-ISS will locate X-ray sources to within 1 arcmin with a limiting sensitivity of 0.1 mCrab in a day. As well as providing an alert facility, the outstanding sensitivity will allow many topics to be studied using Lobster-ISS data alone. Lobster-ISS recently completed an industrial Phase-A study. RSSD staff ensured that the scientific capabilities of the payload were maintained while producing a design that fulfils the requirements of the Columbus External Payload Facility on the ISS. the handful seen so far from ground observatories. The Phase-A study, jointly conducted by the Human Spaceflight and Science Directorates, was recently completed and the final report provided to the ESA Science Advisory Structure. Unfortunately, EUSO was not identified as one of the scientific priorities for implementation in the foreseeable future. Activities are continuing to investigate alternative implementation scenarios. RSSD has supported the Phase-A study by providing coordination between the separate instrument and payload studies, and ensuring that the advice of the independent Science Study Team is properly utilised. 3.1.12 ROSITA ROSITA (Roentgen Survey with an Imaging Telescope Array) is a proposal to perform the first imaging 0.511 keV all-sky survey using an array of telescopes on the ISS. The main scientific goals are to detect obscured accreting black holes, to study the hot intergalactic medium in clusters and the hot gas in cluster filaments, to find distant clusters of galaxies and to investigate the galactic X-ray source populations. Following an initial feasibility study, additional activities are on hold until the outcome of the ‘Dark Universe Observatory’ NASA SMEX proposal is known in 2005. DUO would perform X-ray scans of limited regions of sky, whereas ROSITA would perform an all-sky survey; the science goals of the two missions are somewhat similar. RSSD has provided support to the initial feasibility study and to subsequent discussions with D/HME on future activities. 3.1.13 EUSO Understanding the origin of cosmic rays with energies > 5x1019 eV is one of the primary challenges in astrophysics. At such extreme energies, cosmic rays interact with the cosmic microwave background and the distance that a cosmic ray can travel is limited to our galactic neighbourhood. Intriguingly, all the astronomical objects that could produce such energetic cosmic rays are likely to be much further away. The Extreme Universe Space Observatory (EUSO) will observe the light produced when such a cosmic ray interacts with the Earth's atmosphere. Looking down from the ISS, EUSO could detect around 1000 events per year, compared to http://www.rssd.esa.int/LOBSTER http://www.rssd.esa.int/ROSITA http://www.rssd.esa.int/EUSO sec3.qxd 7/15/05 10:01 AM Page 64 64 3.2 scientific support activities Solar and Solar Terrestrial Missions Division 3.2.1 Introduction and overview The Solar and Solar Terrestrial Missions Division provides scientific support for all ESA missions in solar, heliospheric and solar-terrestrial science. The present missions in operational phase are Ulysses, SOHO, Cluster and Double Star. Solar Orbiter is in its study phase within SCI-A. Apart from providing science support to these missions, the Division is also responsible for their management once in their operational phases. Staff members of the Division are located at ESTEC, with the exception of the SOHO team, who reside at the SOHO Experiment Operations Facility at the NASA Goddard Space Flight Center, Greenbelt, USA. Ulysses has now been in orbit for over 14 years and is presently on its way towards a third set of polar passes in 2006-2007 (south) and 2007-2008 (north), following the decision by SPC to extend the mission to March 2008. Ulysses has also completed a distant encounter with Jupiter, where the scientific highlights were observations of quasi-periodic radio bursts and distant observations of Jupiter dust streams. Ulysses also observed cometary ions in a coronal mass ejection. As in the past, Ulysses’ results continue to feature prominently at international meetings and workshops, and the science team maintains an exceptionally high publication record (over 120 papers during 2003-2004). Such activities are coordinated by the RSSD Project Scientist Team and extend to data dissemination, archives and long-term calibration issues. formations, the Cluster mission continues to deliver outstanding results of small- and large-scale physical processes in near-Earth space. As expected, Cluster has now provided both evidence and direct in situ observations of reconnection in the magnetic tail and the dayside high-latitude magnetopause. It has furthermore confirmed the existence of large-scale boundary waves and vortices at the magnetopause, found filamentary structures in the aurora, the cusp and the tail current, and explicitly measured the extreme thinness of the bowshock and the cross-tail current just before substorm onset. It appears that the number of results from Cluster is still growing at an exponential rate, promising an exciting future. Both SSWG and SSAC have recently taken a positive stand towards plans for a further mission extension to late 2009, allowing a number of new adaptive or multi-scale configurations to be exploited and new magnetospheric regions to be visited (in particular, the important sub-solar magnetopause and the near-Earth tail around 10 RE). An important step in the direction of even more effective Cluster data exploitation was the ESA SPC decision to fund the Cluster Active Archive, an open approach to delivering high-resolution Cluster data to the worldwide community. ESA’s first collaboration with China, the Double Star Project, got underway with successful launches into equatorial (December 2003) and polar (July 2004) orbits. The orbits are designed to support the Cluster mission, and most of the European-provided instruments are identical to the Cluster payload. In spite of some problems with boom deployment and attitude computers, both missions are now operating nominally, and will provide important data complementary to Cluster for at least the mission baseline period of 1 year. The SOHO mission remains the flagship of solar and heliospheric research, continuously supplying scientists and, increasingly, space weather experts, through the RSSD Project Science Operations Team, with data from the Sun. A dramatic incident occurred in mid-2003, when a problem with the high-gain antenna motor resulted in some data loss, which sent a shockwave through the scientific community. Using on-board data storage and clever roll manoeuvres of the satellite, the SOHO RSSD Project Scientist team was able to keep the damage from the malfunctioning motor to a minimum, rescuing continuous helioseismology data even during periods of low-gain antenna contacts. Apart from such problems, SOHO operations and science exploitation have run smoothly throughout the reporting period. As usual, the SOHO RSSD team has been extremely active in science outreach and communications. The most spectacular highlight was the coverage of the extraordinary solar outbursts in Autumn 2003, which are still under scientific study via a large number of spacecraft such as Cluster. After reconfirmation following the reassessment of the Cosmic Vision programme in 2003, Solar Orbiter is under assessment in the Science Payload and Advanced Concept Office, with support from the Study Scientist concerning science issues and contacts with the international scientific community. During 2003, the Solar Orbiter Science Definition team reviewed the scientific goals of the mission, resulting in a wellbalanced and highly focused mission. Probing different key regions of the magnetosphere and solar wind at variable scales using a variety of spacecraft Following the restructuring of the Science Directorate in recent years, no new hardware commitments have been Several instruments built in previous years by members of the Division and SCI-A personnel continue to deliver good data. The instruments presently operative in orbit are COSPIN on Ulysses, LOI on SOHO and EFW and ASPOC on Cluster. For NASA’s STEREO mission, parts of the SEPT/IMPACT instruments were delivered by SCI-A during the reporting period. The SEPT instrument built by SCI-A with science guidance from division staff is the most recent link in a very successful series of energetic-particle instruments from the Division. sec3.qxd 7/15/05 10:01 AM Page 65 scientific support activities 65 taken on during the reporting period. However, it is hoped that staff of the Division will be involved in providing the science requirements and guidance to SCIA for the thermal design and testing of hardware for the ion and electric field instrument on BepiColombo’s MPO and MMO, respectively. Besides the primary occupation of the Divisional staff in supporting the missions in orbit, almost all staff members have pursued their own scientific research. In the absence of new hardware projects, other than those listed above, such activities have now concentrated on data analysis. The prime research fields of the divisional staff are in solar physics (Section 2.5), heliospheric physics (Section 2.6) and space plasma physics (Section 2.6). The combined effort of RSSD staff in scientific data analysis has been supported by an active research fellow programme. Figure 3.2.2/1: An example of quasi-periodic (~40-min period) radio bursts from Jupiter, detected by URAP on Ulysses in October 2003. (Courtesy R.J. MacDowall) 3.2.2 Ulysses Ulysses is an exploratory mission being carried out jointly by ESA and NASA to study the properties of the interplanetary medium and solar wind in the inner heliosphere as a function of heliographic latitude and solar activity. The mission also focuses on the dust and gas components of the local interstellar medium that gain access to the heliosphere inside the orbit of Jupiter. The European-built Ulysses spacecraft was launched by the Space Shuttle on 6 October 1990, and a Jupiter gravityassist in February 1992 deflected it into its final highinclination heliocentric orbit. Major mission milestones to date include the south and north polar passes at solar minimum (1994/95) and again at solar maximum (2000/01). Following a distant encounter with Jupiter in February 2004 and aphelion passage in June 2004, Ulysses is now heading south prior to the third set of polar passes, in 2006/07 (south) and 2007/08 (north). Scientific highlights during the reporting period included observations of quasi-periodic radio bursts from Jupiter, the most distant observations to date of dust streams from Jupiter (Fig. 3.2.2/1), observations of the effects of the October/November 2003 violent solar outbursts at the orbit of Jupiter, and remote observations of cometary ions trapped in a CME (Fig. 3.2.2/2). A joint ESA-NASA Mission Operations Team at JPL conducts spacecraft operations. A major priority during the reporting period was to ensure that critical elements of the hydrazine system used for attitude control remained above freezing. The low temperatures were the combined result of the diminishing power available from the RTG power source and the large distance from the Sun. The ensuing power and thermal constraints required the introduction of a power-sharing plan for the scientific payload whereby a core set of instruments is operated continuously and a subset of the remaining payload is http://helio.esa.int/ulysses Figure 3.2.2/2: Ulysses observes ions from Comet McNaught-Hartley trapped inside a CME. Earth’s orbit is shown for reference. (Courtesy G. Gloeckler) switched on on a rotating basis. Starting in October 2004, the nominal ground station coverage via NASA’s Deep Space Network was reduced from 70 h to 35 h per week. This reduced coverage, introduced as a result of the 2003 Sun-Earth Connections Senior Review in NASA, will last for 2 years. Within these constraints, the spacecraft and payload are operating very well. On the programmatic side, a major achievement was the approval by ESA’s SPC in February 2004 of funding to continue spacecraft operations until March 2008. This mission extension, the third for Ulysses, will enable sec3.qxd 7/15/05 10:01 AM Page 66 66 scientific support activities measurements to be acquired up to and including a third set of polar passes. The scientific rationale for this is the desire to have out-of-ecliptic observations covering as much as possible of a complete Hale (22-year) solar magnetic cycle. Furthermore, the launch in 2006 of NASA’s twin STEREO probes will create a unique opportunity for multi-spacecraft observations during Ulysses pole-to-pole transit in 2007. Funding on the NASA side for 2007-2008 will be decided at a Senior Review in 2006. During the reporting period, the ESA RSSD Mission Manager, together with his JPL counterpart, provided scientific advice to the operations team on all mission aspects and co-chaired the Science Working Team (SWT) meetings. In addition, the Mission Manager cochaired the corresponding ESA-NASA Joint Working Group (JWG) meetings at which the overall policy issues related to the mission are discussed. Four JWG/SWT meetings were held in 2003-2004, two in Europe and two in the USA. A major topic of discussion at recent SWT meetings has been the implementation of payload powersharing. As part of his Project Scientist duties, the Mission Manager assisted in the organisation of special sessions related to heliospheric research at international scientific meetings. Two collections of papers and a major review article, all focusing on the results from the recent solar maximum solar passes, appeared during the reporting period. Individually, the Ulysses investigators continued to publish prolifically, with more than 120 papers appearing in 2003-2004. The Ulysses Data Archive is maintained at ESTEC by a small RSSD Ulysses team and is mirrored at JPL. Ulysses data are also archived by NASA at the National Space Science Data Center (NSSDC), and form part of the Planetary Data System (PDS) archive. During the reporting period, key activities included the acquisition of additional sets of high-resolution time data, and the porting of the archiving software from the current VMS system to Windows and UNIX platforms. 3.2.3 SOHO SOHO is a mission of international cooperation between ESA and NASA to study the Sun, from its deep core to the outer corona, the solar wind and its interaction with the interstellar medium. SOHO has provided the first images of structures and flows below the Sun’s surface and has identified the source regions and acceleration mechanisms of the fast solar wind. It has revolutionised both our understanding of solar-terrestrial relations as well as our space weather forecasting capabilities by providing a continual stream of images of the dynamic solar atmosphere, extended corona and activity on the far side of the Sun. In September 2003 the SOHO Team was presented with Figure 3.2.3/1: Cover of the July 2004 issue of National Geographic, which includes the 32-page story ‘The Sun: Living with a Stormy Star’. the prestigious Laurels for Team Achievement Award of the International Academy of Astronautics (IAA). The award recognises both the outstanding achievements in designing, building and operating the mission, as well as the science it has performed. SOHO is a busy observatory, with many coordinated observations (covering well over half the observation time) involving different instruments as well as groundbased observatories and other spacecraft. The coordination of science operations by the RSSD Project science team focuses on maximising the science output of the mission on both short and long time scales, serving current interests as well as possibilities for future analysis by facilitating requested and ad hoc collaborations. It also involves identification and resolution of technical issues under a variety of operational situations. After showing signs of degradation in May 2003, the azimuth drive of the high-gain antenna was parked in an optimal position in June 2003. Coupled with 180° spacecraft rolls twice per 6-month orbit, the parking position introduces keyhole periods of 2-3 weeks every 3 months, when the low-gain antenna must be used with 34 m or 70 m DSN stations. Low availability of such stations causes about 40% loss of telemetry during such keyhole periods. Careful planning to take full advantage of all on-board recording capabilities has still made it possible to ensure near-continuous time series for the GOLF and VIRGO instruments during the last three keyholes (winter 2003 – autumn 2004), thanks to their http://sohowww.nascom.nasa.gov sec3.qxd 7/15/05 10:01 AM Page 67 scientific support activities doubly redundant telemetry streams. Concurrently, an onboard software patch was developed by Saab Ericsson Space to record only selected telemetry packets. The patch was successfully tested during the last keyhole and will be used for future keyholes, hopefully ensuring continuous helioseismology data from the GOLF, VIRGO and MDI instruments. The Internet-based approach to science operations coordination and data dissemination that SOHO has pioneered since 1994 is still the cornerstone of the SOHO information and data system, and it continues to grow: an average of almost 16 million requests were received, and more than 2700 GB of data were transferred from the SOHO servers every month during the last 2 years (up from 7 million requests and 950 GB during the last period). Over the mission lifetime, the SOHO web servers have received a total of 617 million requests and have delivered > 91 TB of data. Anticipating a reduction in the on-site staffing, emphasis has been placed by the RSSD Project Science team on streamlining all data-handling processes for automation and ease of maintenance. The system encompasses processing, archiving, cataloguing, searching and distribution of level-zero telemetry, ancillary data sets and science processed data, as well as real-time products and general web pages for the public. The SOHO teams have set a new standard in providing images and results through the World Wide Web, capturing the imagination of the science community and the general public alike, and inspiring students of all ages to seek more information about the Sun. SOHO images have become stock footage for news organisations around the world. SOHO maintains its high profile in the international media thanks to continued efforts to improve the SOHO web pages and by expanding the network of personal media contacts. SOHO images were featured on the front covers of many popular science magazines, including the cover of the July 2004 issue of National Geographic, which featured a 32-page story on recent developments in solar science and space weather. Members of the SOHO RSSD Project Scientist Team worked closely with National Geographic staff, reviewing the article and consulting on the artwork and images. 67 and embassy staff, and several film crews making documentaries on the Sun (e.g. Discovery Channel) were supported. 3.2.4 Cluster The four Cluster satellites were launched in pairs on two Soyuz rockets in July and August 2000, into a polar orbit targeting some of the most important near-Earth regions: solar wind, bow shock, magnetosheath, cusp, magnetopause, plasmapause and magnetotail. By providing unique 4-point measurements in the Earth’s magnetosphere, Cluster is revolutionising our understanding of the dynamics of space plasmas. Originally funded to operate for 2 years, and now in an extended mission phase until December 2005, the spacecraft and payload continue to perform well and are expected to do so for several years to come. In order to fully realise the potential of the mission, a second extension will be proposed to the SPC early in 2005. Discoveries made by Cluster have demonstrated the critical importance of making measurements on different spatial scales. For example, the substructure of the magnetopause reconnection layer on electron scales of ~20 km; filamentary structure within the cusp over scales of only 100 km; density irregularities at the plasmapause, including plasmaspheric plumes, over scales from 100 km to several 1000 km; observations of a tail current Figure 3.2.4/1: 3-D cut-away view of Earth’s magnetosphere. The curly features sketched on the boundary layer are Kelvin-Helmholtz vortices observed by Cluster. They originate when the two adjacent flows travel at different speeds; in this case, the magnetospheric flow on one side and the solar wind flow on the other. (Courtesy H. Hasegawa, Dartmouth College) Several special showings of the IMAX film Solarmax were arranged by the RSSD Project Science team, e.g. at the meeting of the American Metrological Society in Seattle and the International Astronautical Congress in Vancouver, Canada. The latter supported ESA’s education support programme at this conference. We have also supported ILWS exhibits at the United Nations in Vienna and New York with SOHO materials, models and real-time images. Numerous VIP tours to the SOHO operations facilities were hosted for European ministers http://sci.esa.int/cluster sec3.qxd 7/15/05 10:01 AM Page 68 68 sheet only ~0.1 RE thick; the scale of the quasiperpendicular shock transition on the ion gyroradius scale; propagating wave modes in the magnetotail with wavelengths of several RE; and huge vortices on the flanks of the magnetosphere. During the last 2 years, the RSSD Project Scientist team has devoted a large part of its time to the operations of the Cluster mission and the distribution of data to the scientific community. It chaired seven Cluster Science Operations Working Group meetings and four Science Working Team meetings. Five Cluster workshops were organised between October 2002 and October 2004, to discuss Cluster data and prepare the plan for the spacecraft separation strategy. A special issue of Annales Geophysicae was published in July 2004 with Cluster results presented during the 5th Cluster workshop in Orleans (F). A special ISSI book is being finalised on Cluster results on the dayside boundaries of the magnetosphere The Cluster Science Data System (CSDS), which has been specially developed to allow fast easy access to the Cluster physical parameters measured by the instruments, has been running smoothly since February 2001. Nine national data centres, in Austria, China, France, Germany, Hungary, Netherlands, Sweden, United Kingdom and the United States constitute the CSDS. They are funded by their national agencies; ESA through the Project Scientist team coordinates the system and provides the user interface to allow a scientific user to query, retrieve and manipulate the data coming from all instruments. User access to the data system is gradually increasing every month. The average download by scientific users over a recent 3-month period was > 5.8 Gbytes/month. The physical parameters database contains more than 30 Gbytes. A Joint Science Operations Centre (JSOC), at the Rutherford Appleton Laboratory (UK), was established to support the Project Scientist in coordinating the complex science operations of the mission. Its five main tasks are payload commanding, payload health monitoring, planning and information dissemination, data management system delivery and maintenance, and the CSDSweb (quicklook) delivery and maintenance. The Cluster quicklook plots are available at http://www.cluster.rl.ac.uk/csdsweb/. JSOC has performed its tasks successfully since the beginning of the mission. A very active period for JSOC is during the constellation manoeuvres, when instruments have to be switched-off during thrusters firing and switched on again afterwards. Constellation manoeuvres consist typically of 50 thruster firings from a few seconds up to more than 1 h during a 1.5-month period and take place once a year. The importance of Cluster data to space physics is underlined by the development of the Cluster Active scientific support activities Archive (CAA), funded by ESA, NASA and member states. From early 2005, this archive will provide free access for the entire scientific community to the full, calibrated, high-resolution Cluster data set (CSDS contains only low- and medium-resolution data). CAA will be a unique research tool for the worldwide magnetospheric science community for many years to come. It consists of a core RSSD team with four people that will prepare and populate the database at ESTEC, and one person in each of the 10 European PI teams to calibrate and deliver the data to the archive. The first CAA data were delivered before the end of 2004 and then 2 years’ worth of data will be delivered annually. 3.2.5 Double Star The two Double Star satellites were launched on 29 December 2003 and 25 July 2004 aboard Chinese Long March 2C rockets. Double Star is a China-ESA programme to study the effect of the Sun on the Earth’s environment. The Chinese National Space Administration built, launched and is operating the two satellites. ESA provided eight European instruments, the support for their integration in Europe, their science operations, and the acquisition of 4 h of data per day using the ESA VILSPA II ground station. The orbits are designed to maximise collaboration with Cluster such that both small-scale and large-scale observations of the magnetosphere are collected simultaneously. The satellites and instruments are working well although a few anomalies occurred shortly after the launches. On TC-1, one solid boom holding the STAFF (magnetic wave detector) did not deploy owing to a problem with a pyro-actuator. STAFF observations are contaminated by a strong background noise. Special software techniques are being developed to minimise this effect. In addition, a strong magnetic disturbance from the spacecraft solar array is observed by the FGM (magnetometer). The FGM software has been modified to limit the effect. On TC-2 the boom pyros were exchanged and the solar panel cabling modified, precautions that avoided the problems encountered with TC-1. Unfortunately, both the main and redundant attitude orbit control computers failed within 2 weeks of launch. This lost the attitude control capability on the polar satellite; however, the attitude can be determined using the European- provided magnetometer data. Spin axis pointing and spin rate are nominal. Although the spin rate is expected to remain stable over the mission, the spin axis is expected to drift slowly. Present drift predictions indicate that at least a 1-year mission lifetime can be achieved for TC-2 without problems. During the last 2 years, the RSSD Project Scientist team, which shares its time with the Cluster project, has devoted a large part of its effort in preparation for the sec3.qxd 7/15/05 10:01 AM Page 69 scientific support activities 69 3.2.6 Solar Orbiter The key mission objectives of the Solar Orbiter mission are: to study the Sun from close up (48 solar radii, or 0.22 AU), permitting investigation of the solar surface at high spatial resolution; to study the links between the solar surface, the corona and inner heliosphere during perihelion passes that are matched to the Sun’s rotation; and to provide images of the Sun’s polar regions from heliographic latitudes in excess of 30°. Solar Orbiter was selected as an ESA Flexi-mission in 2000, and reconfirmed in 2004 to be implemented as a common development with the BepiColombo mission to Mercury. Launch is foreseen for either October 2013 or May 2015. Figure 3.2.5/1: Launch of the second Double Star TC-2 satellite on 25 July 2004 from Tai Yuan. mission, including the science operation of the European instruments and preparation of the data system. The Science Working Team is co-chaired by the Chinese and ESA Project Scientists. The RSSD Project Scientist co-chaired four DSP SWT meetings and four data system implementation working group meetings between October 2003 and October 2004. Since the European contribution to Double Star consists of Cluster spare or duplicate instruments, it was decided to re-use as much as possible the data system developed for Cluster. The European Payload Operation Centre (adapted from Cluster JSOC) updated the data management system for Double Star and coordinates the commanding of the European payload. Similarly, the Double Star Data System (DSDS), a subset of the Cluster data system, distributes data to the user community. The national data centres involved in the distribution of data are in Austria, China, France, The Netherlands and UK. The quicklook plot system has also been adapted to display the data from all instruments, European and Chinese, a few days after data acquisition and is running at the Austrian data centre (http://edds02.iwf.oeaw.ac.at/ dsdsweb). TC-1 operations began in March 2004 and for TC-2 in early October 2004. The coordinated dual satellite mission is planned to last at least until July 2005. The second Double Star workshop took place in Beijing on 8-10 November 2004. More than 50 papers, the majority combining both Double Star and Cluster data, were presented during the 3 days. Very promising results emerged on magnetic reconnection, bow shock structures and surface waves on the magnetosphere. The model payload comprises the following state-of-theart packages of heliospheric in situ and solar remotesensing instruments: Plasma Package (ion and electron solar wind analysers); Fields Package (radio and plasma wave analyser, magnetometer); Particles Package (energetic particle detectors, interplanetary dust detector, solar gamma-ray and neutron detector); Solar Remote Sensing Package (visible-light imager and magnetograph, EUV full-Sun and high-resolution imager, EUV spectrometer, X-ray spectrometer/telescope, coronagraph). In 2003, the Study Scientist formed a Science Definition Team (SDT) that was given the task of reviewing and refining the scientific goals to achieve a well-balanced and highly focused mission. SDT meetings were held in ESTEC in May and September, resulting in a Solar Orbiter Science Requirements Document (Sci-RD), issued in December 2003. Throughout 2004, the Study Scientist supported the assessment activities lead by SCI-A, in particular with respect to payload-related issues, and maintained the interface to the external scientific community. Other activities included presentations at international meetings, and coordination efforts in the framework of NASA’s Living With a Star programme (specifically, Solar Probe and Sentinels), and the International Living With a Star initiative. 3.2.7 Solar-B Solar-B is a solar physics mission, led by ISAS, intended to follow on from the highly successful Yohkoh (Solar-A) mission. The payload comprises a coordinated set of optical EUV and X-ray instruments to investigate the interaction between the Sun’s magnetic field and corona. The final goal is to reach an improved understanding of the mechanisms leading to solar variability and ultimately controlling the energy output. These processes are the main driving forces behind what is generally referred to as space weather. Solar-B is scheduled for a launch in August 2006. After having received an invitation to collaborate with http://sci.esa.int/home/solarorbiter sec3.qxd 7/15/05 10:01 AM Page 70 70 ISAS on Solar-B, particularly on data analysis and operational ground support from a polar station, ESA received SPC approval in early 2003 to invest > 7 Meuro in providing an additional Norwegian ground station on Svalbard. This station, because of its high latitude, will be able to provide downlink for almost all Solar-B passes in its Sun-synchronous low-altitude polar orbit. Closely linked to the provision of the station, ESA is also negotiating with Norway for a European data centre for the full Solar-B database, supplying Europe’s solar physics community with rapid access to the huge amounts of data expected from this mission. ESA’s involvement in Solar-B can be considered as an initial ESA contribution to the International Living With a Star Initiative (ILWS), which aims to increase our understanding of how the variability of the Sun affects the terrestrial and other planetary environments, in the short- and long-terms. In particular, the effects of solar variability on mankind and society are being investigated. B. Fleck acts as the prime ESA contact person with respect to JAXA/ISAS, and R. Marsden and H. Opgenoorth represent ESA in the ILWS steering committee, which has been chaired by the latter for the last 2 years. scientific support activities 3.3 Planetary Missions Division 3.3.1 Introduction and overview The past 2 years were probably the most exciting period for planetary science in Europe, and the staff of the Division played a major role in supporting the community to contribute to this success. Three missions were launched: Mars Express, SMART-1 and Rosetta. Huygens was released from Cassini and completed its mission to study Titan’s atmosphere and surface on 14 January 2005. Venus Express, which was approved end-2002, is in its final stages of testing and will be ready for launch in November 2005. It was a demanding time for the Project Scientists and their teams, supporting the project reviews, monitoring the payload development and testing, and preparing the commissioning activities jointly with the Experiment Teams and the Mission Operations Team at ESOC. The Division is responsible for the coordination of all payload operations for Mars Express, Rosetta and SMART-1. The supporting facilities for these missions have been developed and the various teams have taken over responsibility for planning the operations of their specific mission. In addition to Huygens, the Division took over the responsibility for the mission management, during the exploitation phase, of Mars Express, Rosetta and SMART-1. The launch delay of Rosetta required an additional effort to define the new mission scenario, monitor the new target comet and demonstrate, in a unique team effort with the Project Team and the Rosetta Science Working Team, that we had defined a viable mission to the new target, 67P/Churyumov-Gerasimenko. In addition, the RSSD Project Scientist team had to support a long launch campaign for the second time. The successful redefinition of the baseline mission scenario for BepiColombo by SCI-A was supported by the Project Scientist. Unfortunately, the Mercury Surface Element had to be dropped for programmatic reasons. A successful mission profile involving two orbiters (one ESA and one Japanese) was developed that ensured a major science return could be maintained. The RSSD Project Scientist was heavily involved in maximising this science return from the low-resource model payload designed within SCI-A, as well as in the payload selection process and the accompanying negotiations to secure payload funding. In close collaboration with the Science Operations and Data Systems Division, the ESA Planetary Science Data Archive was created using the tools developed for the archives for ESA’s astrophysics missions. The first data sets ingested were the results from Giotto and the Giotto Extended Mission and from the ground-based observation campaign of the Rosetta targets. The archive sec3.qxd 7/15/05 10:01 AM Page 71 scientific support activities 71 is operational and waiting for the data sets from the first 6 months in Martian orbit from the Mars Express instruments. 3.3.2 Cassini/Huygens The Cassini-Huygens mission is a joint undertaking between NASA, ESA and ASI. It is designed to explore the Saturnian system and all its elements: the planet and its atmosphere, rings and magnetosphere, and a large number of its moons (icy satellites), in particular Titan, Saturn’s largest moon. The Cassini-Huygens spacecraft, launched in October 1997, was placed in orbit around Saturn on 1 July 2004. The interplanetary voyage of 6.7 years included gravity-assists at Venus (April 1998 and June 1999), Earth (August 1999) and Jupiter (December 2000). Results obtained during the cruise phase and the planetary flybys have appeared regularly in the scientific literature. Saturn approach science started in early 2004. It included a coordinated set of observations of Saturn’s auroras by HST while Cassini monitored the solar wind conditions. Remote sensing observations of the entire system during the approach phase allowed the study of what already appears to be a highly variable and dynamic system where all elements are interacting (Saturn and Titan atmosphere, rings, moons, magnetospheric plasma, dust). Nineteen days before Saturn Orbit Insertion (SOI), a 2000 km flyby of the large outer moon Phoebe was performed. Spectacular observations indicated that Phoebe is most likely a captured object from the outer Solar System. During SOI, Cassini-Huygens went through a gap between the F- and G-rings. Unique ring observations were obtained by several remote-sensing instruments, including the Imaging Science Subsystem (two cameras) and various optical spectrometers covering the UV to the far-IR. The fields & particles instrument complement has begun to study the global morphology of Saturn’s magnetosphere. Lightning was detected in Saturn’s atmosphere by the plasma wave sensors, indicating some change in its characteristics since the Voyager observations. By the end of 2004, Cassini had performed three Titan flybys: 2 July (300 000 km closest approach), 26 October (1174 km) and 13 December (1200 km) (Fig. 3.3.2/1). The surface of Titan, ‘seen’ by three remote-sensing instruments (camera, VIMS, radar) is revealing itself to be more complex, exotic and geologically diverse than ever anticipated. The atmosphere’s thick haze is a challenge for the optical remote-sensing instruments in reaching their best resolutions. Remote observations by the Composite Infrared Spectrometer (CIRS) and the Visual Infrared Mapping Spectrometer (VIMS) on 2 July and 26 October, and in situ measurements in the upper atmosphere by the Ion and Neutral Mass Spectrometer http://sci.esa.int/huygens Figure 3.3.2/1: The Cassini-Huygens trajectory on arrival at Saturn. The Huygens mission was carried out on the third revolution around Saturn. Three Titan flybys were achieved before Huygens’ mission: T0 (2 July, closest approach 300 000 km); Ta (26 October, 1174 km); Tb (13 December, 1200 km). The probe mission was carried out on Tc on 14 January 2005. More than 40 Titan flybys are expected to follow Huygens’ mission before the orbiter’s mission ends in mid-2008. (INMS) on 26 October, as well as the two stellar occultation data sets on 13 December by the UV Imaging Spectrometer (UVIS), allowed, in combination with the ground-based data set obtained during the Titan occultation in mid-November 2003, the upper atmosphere model of Titan’s atmosphere to validated and updated, a key step in the validation of the performance of Huygens mission. During the reporting period, the RSSD Mission Manager/Project Scientist, supported by the Huygens Mission Team which is distributed across ESTEC, ESOC, NASA/JPL and Industry, assumed the overall responsibility for the implementation of the Huygens recovery mission, which was completed in December 2003 when the required Probe onboard software patches were uploaded and validated. In 2004, the work concentrated on preparation activities for the Huygens mission itself. Three major Huygens reviews were conducted in 2003-2004. An Agency-wide Delta Flight Acceptance Review was conducted on the recovery mission from December 2003 to February 2004. The review identified the need to consolidate the entry heat flux and heat load calculations, because recent work on radiation flux during entry into a methane-rich nitrogen atmosphere had raised questions on the work done in the early 1990s. A special effort began in April 2004 with the Huygens industry team, NASA and Ecole Centrale de Paris, where there is unique expertise high-temperature plasma radiation spectroscopy. The work concluded in late November 2004, allowing the latest methane sec3.qxd 7/15/05 10:01 AM Page 72 72 Figure 3.3.2/2: Updated Titan atmosphere profile after the T0, Ta, Tb flyby data set. The update profile, represented by he thick purple line, falls within the envelope of the engineering model used for the Huygens mission design. concentration in Titan’s atmosphere derived from the early Cassini observations to be taken into account (Figs. 3.3.2/2 & 3.3.2/3). An ESOC-led Delta Ground Segment Readiness Review was held in September 2004. The recertification of the entry performance was one of the major topics addressed in a Joint ESA/NASA Mission Risk Review (MRR), which was conducted from midOctober to mid-December 2004. The MRR gave the green light, on 16 December, to proceed with preparations for the probe’s release. Huygens was successfully released from Cassini on 25 December 2004 at 02:00 UTC. Thanks to excellent pointing and performance of the Spin and Eject Device, Huygens was targeted at the nominal entry angle of –65º. A series of optical navigation images of the probe was obtained by the two Cassini cameras, which contributed to refining the probe trajectory and to confirming that the entry ellipse uncertainty was only 0.8º (3º requirement). At the end of 2004, it was known that Huygens was well on its way to Titan for an entry on 14 January 2005 at 09:06 UTC (Fig. 3.3.2/4). Following an initial study within the ESA General Studies Programme (GSP) in mid-2003, initiated by the Technical Directorate, a project was developed for tracking the probe using Very Long Baseline Interferometry (VLBI). The objective of the study was to investigate synergies available between large effective apertures for radio astronomy and the needs of space applications like data downlinks (MARS/Venus/ Mercury landers and/or small orbiters) and monitoring scientific support activities Figure 3.3.2/3: VIMS image of Titan after Ta observations. The expected Huygens landing site is shown. space debris. In order to arrive at a realistic concept, the study focused on the tracking of Huygens during its descent to Titan. The initial study was closely followed by the RSSD Project Scientist. It demonstrated that the tracking of Huygens was achievable. Following the positive outcome of the initial study, further work was done jointly by the Technical and Science Directorates to develop a project for Huygens VLBI observations. The ESA studies were led by the Joint Institute for VLBI in Europe (JIVE), in Dwingeloo (NL). The main goal was to measure the position of the probe during its descent and on the surface to an accuracy of the order of 1 km with a time resolution of a few seconds. At the initiative of JIVE, radio telescope time was applied for and obtained as part of the regular AO process in the US and in Australia through peer-review proposals, which were highly ranked during the evaluation process. Altogether, 18 telescopes in the USA, Australia, Japan and China were involved in the observations. Two test observations were conducted in late August 2004 (using Cassini transmitting in the X-band as the RF source), and in mid-November 2004 (using Cassini’s Radio Science S-band transmitter and Mars Express’ S-band transmitter). Those test observations allowed the Huygens team to debug and coordinate the complex observation plan and were key to preparing for the real Huygens observations. Huygens successfully landed on Titan on 14 January 2005. All science instruments performed well, yielding a data set of the moon’s physical and chemical properties. The amazing descent panorama and superb pictures from the landing site can be found on http://saturn.esa.int or http://saturn.jpl.nasa.gov sec3.qxd 7/15/05 10:01 AM Page 73 scientific support activities 73 Operations Centre (RSOC) and have a fully operational system ready for the payload commissioning that started shortly after launch. It is responsible for consolidating the command sequences for the operation of the science payload. These command files are submitted to the Rosetta Mission Operations Centre (RMOC) at ESOC. In addition, the Project Scientist Team team supported all Project Reviews and the official RSOC Reviews as part of the Rosetta Ground Segment validation and commissioning. Figure 3.3.2/4: Huygens Entry, Descent and Landing scenario. 3.3.3 Rosetta On 2 March 2004 Rosetta was launched from Kourou on an Ariane-5G+. After the delay from early 2003 owing to the failure of the new Ariane-5ECA, the Project and the RSSD Project Scientist team, in close collaboration with the Rosetta Science Working Team, studied alternative mission scenarios. These had to meet three basic requirements: preserve the scientific objectives of the mission, minimise the technical risks, and minimise the financial impact on the overall Science Programme. A mission to comet 67P/ Churyumov-Gerasimenko was finally identified that met these requirements. The RSSD Project Scientist team, in collaboration with the scientific community, mounted an observing campaign to characterise the new target in support of defining the new mission scenario. In parallel, technical activities proceeded at an increased pace in order to meet the new launch date of February 2004. Fortunately, the Rosetta orbiter did not require changes to cope with the new mission scenario. However, considerable effort was needed to demonstrate the compatibility of the Philae Lander design with the new target. Churyumov-Gerasimenko has a radius of 2 km, in comparison to the 0.6 km radius of the original target 46P/Wirtanen. The greater gravitational attraction will produce a higher touchdown speed on the nucleus. All these technical hurdles were overcome and Rosetta was ready to be launched at the end of February 2004. After two brief launch delays due to bad weather and a technical problem, respectively, Rosetta was finally launched. The Project Scientist team used the 1-year delay to improve the implementation of the Rosetta Science http://sci.esa.int/rosetta/ The payload commissioning was split into three periods – two periods immediately after launch until early June – and the Pointing and Interference Campaigns in September and October 2004. For the last period, RSOC took for the first time full responsibility for preparing the payload operations. This required very close interaction and collaboration with the Experiment Teams. The system worked flawlessly and proved the readiness of RSOC. The Mission Commissioning Results Review on 3 December 2004 at ESOC concluded that all goals of the spacecraft and payload commissioning had been achieved and that the mission was operational. From mid-October the spacecraft was in quiet cruise mode, the next big event being the first Earth gravity assist on 4 March 2005. Subsequently, for the operational phase of the mission the management of Rosetta was transferred from the Projects Department to RSSD. 3.3.4 Mars Express Mars Express is ESA’s first planetary mission and was launched on 2 June 2003 from Baikonur Cosmodrome aboard a Soyuz-Fregat. Following a 7-month journey, it was inserted into Mars orbit on 25 December 2003. The Beagle 2 lander was released on 19 December and should have landed on 25 December; it was considered to be lost following extensive searches by the NASA Mars Odyssey orbiter, terrestrial radio telescopes and Mars Express itself. The Mars Express orbiter is designed to achieve the following science objectives: — — — — global high-resolution (10 m) photogeology; super-resolution imaging at 2 m/pix of selected areas; global mineralogical mapping at 100 m resolution; global atmospheric circulation and mapping of composition; — study subsurface structure at km-scale down to the permafrost; http://sci.esa.int/marsexpress/ sec3.qxd 7/15/05 10:01 AM Page 74 74 scientific support activities — study surface-atmosphere interactions; — study interaction of the upper atmosphere with the solar wind. The RSSD Payload Support Team (PST) at ESTEC acts on behalf of the RSSD Mission Manager, in consultation with the Science Operations Working Group (SOWG). The Mission Manager is advised by the Project Scientist and the Science Working Team (SWT) on all matters related to optimising the mission’s scientific return. The SOWG is composed of PI team representatives assigned to address all science operations issues. The Payload Operations Service (POS) at RAL (UK) is contracted to support the PST, the PIs and the Mission Operations Centre (MOC) in conducting efficient operations of the mission’s scientific instruments. The POS develops, implements, tests and operates the system and tools required to support Mars Express. For the detailed planning and the transition to and implementation of the commanding of each instrument’s operations, POS interfaces with the MOC on one side, and with the PI institutes on the other. The PST plays a key role in coordinating all the required inputs, respecting the mission constraints and safeguarding the balance in the scientific return of the Mars Express instruments. Up to the launch, the PST focused on preparing for mission science planning and operations. A large effort was spent on preparing the Master Science Plan, a document describing the full range of Mars Express science goals and mission planning, from global overview to full detail. Following launch, emphasis shifted to understanding and coordinating the mission and its constraints in order to arrive at an efficient and optimised mission planning process. This also involved the first example of ‘interplanetary networking’, in which some data from the NASA Mars rovers were routed through Mars Express to Earth. The PST has also been active in preparing the requirements for the Mars Express science archive. It was decided that the best way to implement the archive would be through the reuse of the technology and software used for ISO (and later XMM-Newton). The archive was expected to be online in early 2005. 3.3.5 Venus Express The development of the Venus Express (Fig. 3.3.5/1) mission is progressing well and is on schedule for a launch on 26 October 2005. The spacecraft is based on the Mars Express platform, with modifications to the thermal control to handle the more challenging environment around Venus. The solar panels have been redesigned and now use modern-technology cells that Figure 3.3.5/1: Venus Express in fully operational configuration. As the solar input at Venus is about twice that at Mars, the solar panels are shorter than for Mars Express. operate well at the high temperatures expected at Venus, and the size of the panels has been halved. The payload is composed of a selection of instruments from Mars Express, Rosetta and two newly built instruments. Venus Express will be launched from Baikonur Cosmodrome by a Soyuz-Fregat into a direct transfer trajectory to Venus. The journey to Venus requires about 150 days. The operational orbit is a highly elliptic 24 h polar orbit, with a pericentre altitude of 250-350 km and an apocentre altitude of 66 000 km. The observations will be split between the pericentre region, where highresolution studies of small-scale features will be carried out, and near-apocentre and intermediate observations, where global features will be studied. Activities within the Planetary Missions Division have concentrated on three areas. The first is the organisation and lead of the Science Working Team and the related meetings, with, as an important result, the refinement of the scientific objectives and the definition of principles for selecting observations for the different phases of the mission. The second is the definition and the set-up of the Science Operations Centre within the Division. The third is interfacing with the ESA project team, ESOC and the industrial contractors to follow the development of the different elements of the project closely. A somewhat new top-down approach has been taken to the formulation of the scientific objectives. The objectives are formulated as a set of fairly wide fields of interest or ‘themes’, where each theme is broken down into several sub-themes. The sub-themes in turn, are broken down into a set of observations to be made, where the physical parameters to be observed are defined. The observations are distributed over the different phases of the mission based on the importance of the specific http://sci.esa.int/venusexpress/ sec3.qxd 7/15/05 10:01 AM Page 75 scientific support activities 75 conditions like illumination, repetition rate, conjunctions, eclipses and available downlink capability. For each phase, all measurements that address all aspects of the defined observations, and the individual instruments that make the measurements, are identified. In this way, full traceability exists in both directions: it can be seen directly which theme is addressed by a specific measurement and it can be verified that each theme is properly covered with an adequate set of measurements. The following Science Themes have been defined, — — — — — — — Atmospheric Dynamics; Atmospheric Structure; Atmospheric Composition and Chemistry; Cloud Layers and Hazes; Radiative Balance; Surface Properties and Geology; Plasma Environment and Escape Processes. The organisation of the Venus Express Science Operations Centre (VSOC) has been defined and its interfaces to ESOC and to the individual PI institutes are in the final state of definition. Experience from previous missions, in particular Mars Express, Rosetta and SMART-1, is used to synthesise a design that is flexible and maximises the efficiency of the limited resources available. A generic software package, MAPPS (Mapping and Planning for Payload Science) for assisting in the planning process is under development in-house. A first version was distributed to the PIs and other potential users during a dedicated workshop. The intention is that this package will contain all functions needed for the planning the science observations. It reads the individual instrument request files, analyses and checks the required resources and produces the files that are passed to ESOC for further transmission to the spacecraft. The project has been progressing at an unprecedented pace since the start in 2002. The RSSD Project Scientist team has interacted with the project team, ESOC and industry by participation, mainly by the Project Scientist, in numerous meetings and by closely following and commenting on the progress. The areas of payload development, accommodation and operation, and spacecraft performance and operations have been prioritised. In some cases, when of direct interest to the science performance, the performance and characteristics of spacecraft subsystems have been monitored. Contribution has been made to all major agency-level reviews for spacecraft and ground system, as well as to all payload reviews. 3.3.6 BepiColombo BepiColombo is an interdisciplinary mission to explore Mercury through a partnership between ESA and JAXA. The mission was selected and approved by ESA’s SPC in Figure 3.3.6/1: An example of the MMO and MPO forming part of the BepiColombo composite stack together with the SEPM and CPM. October 2000 as the 5th Cornerstone mission. The Mission consists of two orbiters, the Mercury Planetary Orbiter (MPO), which is 3-axis-stabilised and nadir pointing, and the Mercury Magnetospheric Orbiter (MMO), a spinning satellite. The MMO is being provided by JAXA. ESA is responsible for the overall BepiColombo mission design, including launcher, spacecraft composite, propulsion modules, ground segment and the delivery of both spacecraft into their dedicated orbits, as well as for the MPO and its operations. The severe reduction of the science budget after the Ministerial Conference in November 2001 resulted in a mission reassessment process, which started in October 2002 with the aim of maximising the scientific performance through the optimisation of the payload complement, while reducing costs and programmatic risk. The reassessment was performed by SCI-A in close cooperation with the Planetary Missions Division (SCI-SB), and was completed in June 2003. The mission scenario that emerged from the reassessment was to carry the MPO and MMO together on a single launcher (Soyuz-Fregat 2-1B) in mid-2012 (Fig. 3.3.6/1). The transfer to Mercury will be based on Solar Electric Propulsion with a travel time of about 4.6 years. Upon arrival, the Solar Electric Propulsion Module (SEPM) will be jettisoned and the Chemical Propulsion Module (CPM) will provide the required thrust for Mercury capture and orbit insertion (Fig. 3.3.6/2). The orbiters are dedicated to the detailed study of the planet and its exospheric and magnetospheric environment. The MPO investigations include high-accuracy measurements of the planet’s interior structure and a global multi-wavelength analysis of the surface at a http://sci.esa.int/bepicolombo/ sec3.qxd 7/15/05 10:01 AM Page 76 76 Figure 3.3.6/2: MPO and MMO orbiting Mercury. resolution of 500 m, providing its morphology as well as elemental and mineralogical composition. Thus surface morphology will be correlated with surface composition. Together with the MMO, it will provide the detailed structure of the magnetic field and a complete characterisation of Mercury’s exosphere. The MPO orbit produces optimal coverage of the polar regions. Hence the material of the radar-bright spots observed from Earth and suspected to be either water ice or sulphur will be identified. The detection of sulphur would strongly support the presence of at least a partially molten core. At the start of the reassessment the Project Scientist, in close collaboration with the external Science Advisory Group, formulated the detailed science requirements for the MPO scientific payload. In cooperation with the science community, these agreed requirements were then translated by SCI-A personnel into requirements on instrumentation, which served as the basis for the development of the overall payload architecture. Specific science teams coalesced around particular themes of MPO measurements, such as imaging, IR-spectroscopy/ radiometry, laser altimetry, UV/X-ray/gamma-ray/ neutron spectroscopy, radio science, magnetic field and particle measurements, in order to develop the scientific thrust of the mission. This effort resulted in a rather novel payload concept based on a high level of integration. The resultant MPO reference payload no longer consisted of individual instruments, but of the front ends of these instruments (IFE), which share common subsystems such as data processing, electronics and power. In addition, advantage was taken of the fact that new technologies and miniaturisation techniques have been developed in recent years, which allow alternative approaches in instrument design and increased performances with lower use of precious resources (mass, power, etc.). This new payload concept led to a significant reduction in the mass of the reference payload which in turn allowed for the inclusion of additional instruments (thermal-IR mapping spectrometer and radiometer, scientific support activities neutral and ion particle analyser, limb pointing camera, magnetometer), thereby maximising the mission’s overall science return. Considerable effort by the RSSD Project Scientist team went into further optimising this scientific return by ensuring that specific measurements from individual instruments could be correlated and would complement each other. An example of this approach is the correlation of the surface morphology based on the optical camera instruments with the mineralogical and elemental composition of individual surface features as derived from the IR and X-ray imaging spectrometers. In addition, simultaneous measurements from the MPO and MMO will resolve spatial and temporal ambiguities in the exosphere and magnetosphere that would arise from single-point observations. In November 2003 the SPC approved this new concept for MPO payload procurement through the endorsement of the BepiColombo Science Management Plan. As a result, the Request for Proposals for IFEs was issued on 26 February 2004; 20 proposals for the MPO payload were received. On 30 September 2004 the Payload Review Committee recommended an MPO payload complement for selection that reflects the Reference Payload. Considerable effort by the Project Scientist was required in support of the Payload Review Committee and subsequent negotiations with national funding agencies and potential instrument consortia. As a result, with the payload selection process now complete and the mission deep into its definition phase, BepiColombo is now well placed for a launch in mid-2012. Arrival at Mercury and the start of the science exploitation phase is expected for early 2017. 3.3.7 SMART-1 SMART-1 was launched by Ariane-5 on 27 September 2003. The commissioning of the spacecraft, its ion engine and instrument functional checks were completed during the first few weeks after launch. SMART-1 had to travel through the inner radiation belts, during which very violent solar flares in October-November 2003 made the operation of the startrackers and the ion-driven spacecraft very difficult. The instruments were commissioned in February 2004 and the first images and spectra from the Earth and the Moon were obtained. After an eclipse period in March 2004, the spacecraft expanded its spiral towards the Moon, until the lunar resonant approaches on 19 August (when SMART-1 was closer to the Moon than to Earth for the first time), on 27 September and again on 12 October 2004. SMART-1’s science objectives include studies of the chemical composition of the Moon, of geophysical processes (volcanism, tectonics, cratering, erosion, deposition of ices and volatiles) for comparative planetology, and high-resolution studies in preparation sec3.qxd 7/15/05 10:01 AM Page 77 scientific support activities 77 Figure 3.3.7/2: Images taken by SMART-1 during the lunar approach phase. The right image shows a slice of the Moon’s far side and north pole; this was seen for only the second time in the history of lunar exploration. Figure 3.3.7/1: First image of Europe obtained by AMIE, from 70 000 km in July 2004. This began a series of synoptic Earth images for camera operation validation and calibration. for future lunar exploration. The results could provide new insights into topics such as the accretion processes that led to the formation of rocky planets, and the origin and evolution of the Earth-Moon system The SMART-1 science payload, with a total mass of 19 kg, features many innovative instruments and advanced technologies such as a miniaturised highresolution camera (AMIE) for lunar surface imaging, a near-IR point-spectrometer (SIR) for lunar mineralogy investigation, and a very compact X-ray spectrometer (D-CIXS) with a new type of detector and microcollimator that will provide fluorescence spectroscopy and imagery of the Moon’s surface elemental composition. The cruise and lunar approach demonstrated a number of technologies (spacecraft, navigation, operations and instruments) that will be useful for the future. The mission’s prime objective, to demonstrate Solar Electric Propulsion, has been fulfilled. The RSSD Project Scientist and support team, together with the Science and Technology Operations Coordination (STOC) centre at http://sci.esa.int/smart-1/ Figure 3.3.7/3: Mosaic view of crater Pythagoras taken by AMIE on 29/30 December 2004 from an altitude of 4000 km. ESOC, have been planning payload operations for the cruise phase and the first part of lunar phase. The SIR IR spectrometer showed nominal performance when it measured the first near-IR space spectra of the Moon in the range 0.9-2.5 µm. It also measured, by comparison, Earth reference spectra with atmospheric absorption. The comparison between lunar spectra has demonstrated the ability of the instrument to distinguish the mineralogy of different areas on the Moon. AMIE has achieved a number of Earth pointings (Fig. 3.3.7/1) which have been used not only for educational and outreach purposes, but also to measure sec3.qxd 7/15/05 10:01 AM Page 78 78 scenes of planetary interest using various colour filters (geologic features such as volcanic terrains). It has also observed the Moon at different distances and phases to validate the instrument performances and exposure times (Fig. 3.3.7/2 & 3.3.7/3). The Project Science team has been heavily involved in the planning and execution of these operations during this early preparatory phase. SMART-1 has been the only mission in lunar orbit since it was captured by the gravity field on 15 November 2004. Beyond its remaining primary science objective, the mission provides, both for ESA and Europe, an excellent strategic position from which to contribute to future international lunar exploration collaborations with approved missions (Lunar-A, Selene, Chandrayaan-1, Chang’E, Lunar Reconnaissance Orbiter, Moonrise), and possibly within the framework of the new NASA Exploration initiatives. By the end of 2004, more than about 110 papers related to SMART-1 had been published in the scientific literature, including 23 refereed papers. There is a large public interest, as indicated by the media response, articles and the web presence that showed Europe-wide visibility for SMART-1 science and technology. scientific support activities 3.4 Fundamental Physics Missions Division 3.4.1 Introduction and overview The main activities in the Fundamental Physics Missions Division fall into three areas: direct detection and observation of gravitational waves, high-precision tests of the Equivalence Principle (EP), and fundamental physics applications of laser-cooled atoms. In the first area, two missions are supported by the Division: LISA (Laser Interferometer Space Antenna) and LISA Pathfinder (formerly SMART-2). LISA is a mission to detect and observe gravitational waves, jointly undertaken with NASA. LISA Pathfinder is a technology mission, aimed at demonstrating and validating key technologies for LISA. During most of the reporting period both missions were supported by an RSSD Project Scientist. In July 2004, ESTEC hosted the 5th International LISA Symposium, organised by the LISA Project Scientist. Various other workshops and meetings associated with LISA and LISA Pathfinder took place during the reporting period. In the second area, the Division supports the Microscope mission. This is a CNES/ESA collaborative mission to test the EP in space, with a launch by the end of 2007. The third area includes the Atomic Clock Ensemble in Space mission. ACES is under development for flight aboard the ISS, led by the Directorate of Human Spaceflight, Microgravity & Exploration (D/HME); the Division provides support in the form of a Project Scientist. 3.4.2 LISA Pathfinder (formerly SMART-2) LISA Pathfinder (LPF) is primarily intended to demonstrate the key technologies for the LISA mission, especially the performance of the inertial sensors that cannot be tested on the ground. To this end, LPF will accommodate a LISA Technology Package (LTP), provided in large part by European institutes and industry, and a Disturbance Reduction System (DRS) that is very similar to the LTP and has the same goals but is provided by US institutes and industry. LTP and DRS will be accommodated on a single spacecraft, injected into an L2 halo-orbit. The projected mission duration is 180 days, shared between LTP, DRS and a joint operational mode. The mission goals for the LTP are: — demonstrating drag-free and attitude control in a spacecraft with two proof masses in order to isolate the masses from inertial disturbances. The aim is to demonstrate a performance on the order of 10–14 m/s2/Hz1/2 in the frequency band 1-100 mHz. The corresponding requirement for LISA is 10–15 m/s2/Hz1/2; sec3.qxd 7/15/05 10:01 AM Page 79 scientific support activities 79 — demonstrating the feasibility of performing laser interferometry in the required low-frequency regime with a performance as close as possible to 10–12 m/Hz1/2 in the frequency band 1-100 mHz, as required for LISA; — assessing the longevity and reliability of the capacitive sensors, thrusters, lasers and optics in the space environment. As the environment of the LPF spacecraft will be comparatively noisy (in terms of temperature fluctuations and magnetic disturbances) compared to the LISA environment, the mission goal for LPF is to meet a performance of the inertial sensor that is a factor of 10 more relaxed than is required for LISA. This will allow validation of the models derived and extrapolated from ground testing, and further extrapolation to the LISA requirements. The LTP represents one arm of the LISA interferometer, the distance between the proof masses is shrunk from 5 million km to 20 cm. As in LISA, the proof masses fulfil a double role: they serve as optical references (‘mirrors’) for the interferometer, and as inertial references for the drag-free control system. The drag-free control system aboard the LTP consists of the inertial sensor, a propulsion system and a control loop using capacitive sensing in all six degrees of freedom, as well as the interferometric readout system. After completing the two parallel system-level industrial studies in 2003, both of which were actively supported by the Project Scientist. the implementation phase began in May 2004. A major milestone was passed by the successful completion of the System Requirement Review (SRR) in November 2004. 3.4.3 LISA The objective of the LISA mission is the detection and observation of gravitational waves from super-massive black hole coalescences and galactic binaries in the frequency range 0.1-100 mHz. The mission includes three identical spacecraft, located at the vertices of an equilateral triangle with a baseline of 5 million km. The centre of the triangle is in the plane of the ecliptic, 1 AU from the Sun, and trailing Earth by about 20º. By measuring the distance between the spacecraft interferometrically, the effects of a passing gravitational wave can be registered. The orbital motion of the detector allows information about the position and orientation of the gravitational waves’ sources in the sky to be obtained. The scientific goals of LISA are: — determine the role of massive black holes in galaxy evolution; — make precision tests of Einstein’s Theory of Relativity; http://sci.esa.int/lisa/ — determine the population of ultra-compact binaries in the Galaxy; — probe the physics of the early Universe. LISA is an ESA/NASA collaborative mission with a launch foreseen in the 2012-2013 timeframe. By the end of 2004, the project had entered the formulation phase (Phase-A), both in Europe and in the US. As a means of ensuring good communication between the engineers and scientists, regular meetings involving both sides take place. They are held typically three times per year, alternating between the involved centres, ESTEC, GSFC and JPL. The RSSD Project Scientist and his US counterpart coordinate this activity. To develop the requirements and design for the mission and oversee the definition and development, helping to make trade-offs and mission design choices, NASA and ESA formed a LISA International Science Team (LIST) in early 2001. LIST has 11 European and 11 US members, including the respective Project Scientists. As the project entered mission formulation at the end of 2004, LIST met for the last time in December 2004 before being disbanded. The science team will be reinstated with modified membership and charter in 2005 to support the mission formulation phase. In July 2004, ESTEC hosted the biennial International LISA Symposium, organised by the RSSD Project Scientist. The Symposium attracted over 160 scientists; about 80 papers and posters were presented. 3.4.4 ACES The Atomic Clock Ensemble in Space (ACES) mission consists of a caesium-atom clock and a hydrogen-maser clock aboard the ISS, plus laser and microwave links to ground stations. It is managed by D/HME; the RSSD Project Scientist provides scientific support and SCI-A has assisted in technical development and programmatic issues. The ACES atomic clocks will be used as high-sensitivity sensors for experimental tests of general relativity. The mission will contribute to fundamental physics experiments in two distinct areas: — an improved measurement of the redshift by comparing ultra-stable clocks aboard the ISS and the ground. The expected improvement over Gravitational Probe-A is a factor 25. A number of auxiliary measurements, such as a high-precision test of the Sagnac effect and the search for a possible anisotropy of the one-way speed of light (the theory of special relativity), can be performed with significantly improved precision; — the search for a possible drift of the fine structure constant. This constant characterises the strength of sec3.qxd 7/15/05 10:01 AM Page 80 80 scientific support activities the electromagnetic interaction. The principle of the experiment is to compare the rate of atomic clocks (using different elements) as a function of time. Another test of relativity is to search for a possible anisotropy in the one-way propagation of light. The comparison of ACES clocks with ground clocks distributed worldwide will involve propagation of electromagnetic waves (both optical and microwave) in very different directions. 3.4.5 Microscope Microscope (MICROSatellite à trainee Compensée pour l’Observation du Principe d’Equivalence) will be the first mission to test the EP in space. The accuracy is 10–15, 2-3 orders of magnitude better than possible on the ground or with lunar ranging. The payload comprises two differential electrostatic accelerometers, one testing a pair of identical materials (to provide an upper limit for systematic errors), one testing a pair of different materials (the EP test proper). The test masses are freely falling concentric cylinders of platinum and titanium, respectively. A violation of the EP would manifest itself as a differential movement of the proof masses with the orbital frequency of the satellite. The 3-axis stabilised, 193 kg satellite is planned for launch in November 2007 on a shared Dnepr rocket into a Sun-synchronous, quasi-circular orbit at about 700 km altitude. The drag by the residual atmosphere at orbital altitude and solar radiation pressure will be compensated by a drag-free control system using Field Emission Electric Propulsion (FEEP) thrusters. The required dragfree performance is 3x10–10 m/s2/Hz1/2 in the measurement bandwidth. Microscope is a CNES/ESA collaboration: ESA’s share is the procurement of the FEEP thrusters. In return, ESA will have full access to all FEEP flight data, which will provide a valuable technology test in space for a whole suite of future astronomy and fundamental physics missions. 3.5 Space Telescope Operations Division The Space Telescope Science Institute (STScI) is responsible for all aspects of HST operations and, in particular, its scientific productivity. The Space Telescope Operations Division of ESA contributes to this effort with the assignment of 15 ESA staff scientists and engineers. Some of the senior staff members have achieved significant leadership roles within the Institute’s structure and are influential in key areas of the decision-making process. In addition, activities in support of the Hubble programme are carried out at the ST-European Coordinating Facility in conjunction with ESO. The Division manages and leads these activities. The Hubble programme is considered to be one of the most effective science missions ever, as rated by citations in science news media. It has one of the most recognised names and it is routinely cited as a major reason for increased worldwide interest in astronomy. The demand for telescope time is at a record high: more than six times as much time was requested in Cycles 12 and 13 than was available. Highlights of the HST programme include notable enhancements in Hubble’s ability to produce world-class science, along with several achievements that gained worldwide attention. By every measure, HST has more science capability now than at any time in its lifetime. It has achieved a discovery power 10 times greater than at the beginning of the reporting period; ESA staff contributed to all phases of this improvement. The year of 2003 began with the tragic loss of the Space Shuttle Columbia and its crew of seven on 1 February. It ended with Hubble returning data of unprecedented quality and size as a result of the instrument upgrades made by Columbia’s crew on its last mission before the disaster, Servicing Mission 3B. In between, we saw the continued growth of new ideas to use Hubble to understand the cosmos, stimulated by its evolution as the world’s only serviceable space telescope. Hubble was designed for an entirely different set of scientific problems than those it is solving now. Most of the original problems were solved in Hubble’s first decade, and it is now concentrating on the most important topics of today, none of which was developed or even imagined during Hubble’s design. Yet Hubble is now a dominant force in these new topics, in some cases uniquely so. A primary responsibility of the Institute, and an activity led by RSSD staff, is to optimise the HST science programme. There are several major areas where the Institute adds value to the Hubble science programme, and these are naturally the focus of our improvement activities. These include stimulating the best possible science programme from the astronomy community via http://ecf.hq.eso.org/ sec3.qxd 7/15/05 10:01 AM Page 81 scientific support activities 81 the proposal selection process, achieving the highest possible observing efficiency with the telescope, providing timely and accurate calibration of the Hubble data, stimulating the use of the Hubble data archive for additional scientific results, and providing tools to support the astronomical community’s use of the telescope and the archive. Programs were selected and some are already fully completed. As an example, investigators from programmes such as the Great Observatories Origins Deep Survey have already published more than 30 papers describing their results in prestigious journals. The high quality of papers based on Hubble observations reflects the high degree of competitiveness of the proposal process. 3.5.1 HST observation programme Another important change was the start of the Hubble Theory Program, funded as part of the Hubble Archival Research programme. The Theory Program stressed the importance of promoting theoretical research in conjunction with major observing facilities, in order to improve the interpretation and understanding of the data from these facilities. 2004 saw continued evolution in the process for selecting the Hubble science programme. Major improvements were made, starting with Cycle 12, by reducing the time between submitting proposals and starting observations in an observing cycle. The Phase I deadline was moved from September to the end of January, with observations starting in July. Shortening the time between proposal deadline and cycle start helps to ensure that recent findings have greater influence on new Hubble observations, quickening the pace of scientific advance. Observatory operations continued at high efficiency, averaging 43.7% for prime science observations and 48.6% for prime plus snapshot observations. Almost 60% of Hubble’s observing time in the current cycle uses the Advanced Camera for Surveys (ACS), installed during SM3B in April 2002. The science data rate increased by more than a factor of two following the installation of the new instruments and the ground system has been upgraded to respond to this increase challenge. HST is also becoming easier to use, thanks to the new tools produced at the Institute; migration of the archive data to magneto-optical media was completed in 2004. Several new software tools in support of HST operations were released: the Astronomer’s Proposal Tool (APT), StarView and the Space Telescope Grant Management Systems (STGMS) are fully operational. These activities involved considerable effort by RSSD staff. 3.5.2 Special HST programmes STSci and, in particular, the ESA staff have provided leadership in several important science policy issues. Two new programmes, Treasury and Theory, added opportunities for scientists to do research with Hubble and its data archives. The Hubble Treasury Program was started in Cycle 11 to stimulate science that might not naturally be encouraged by the existing process, and, in particular, to promote the creation of important data sets that one would regret not having obtained when Hubble is ultimately decommissioned. Treasury programmes address multiple scientific problems with a single, coherent dataset. The data sets carry no proprietary rights. Recently compiled metrics support the conclusion that papers from larger programmes, such as the Treasury Programs, have considerably higher scientific impact than those from smaller programmes. Several Treasury A successful policy-related topic has been the implementation of the project to trade observing time between Chandra and HST. Both the HST and Chandra Time Allocation Committees and users are very supportive of the concept. 3.5.3 Instrument status With the demise of the imaging spectrograph (STIS), there has been renewed interest in the slitless capabilities of ACS, particularly in the UV. In-orbit calibration data are being reduced and a further calibration programme is being planned to ensure that users are able to obtain highfidelity spectra from these modes. Wide Field Camera 3, planned to be installed in HST in the next servicing mission, is undergoing ground testing and ECF is involved in the testing of the three grisms, one for the near-UV and two for the near-IR. The possibility of applying the extraction software to FORS2 MXU data is currently being investigated and some daytime calibrations have been taken to determine the feasibility of this approach. Under the Extension of the NASA/ESA MoU on HST, the Instrument Physical Modeling group continued the work on upgrading the HST STIS calibration pipeline (STIS-CE) with physical model-based modules. This work is the consistent further development of the idea that calibration should make use of all the a priori information that is available from the physical principles that are embedded in the instrument’s design and construction. Earlier testimony to the advantages of this concept is the stability of the ESO VLT UVES pipeline and the several solutions provided for calibration shortcomings of the HST FOS spectrograph. 3.5.4 The European Coordination Facility The Hubble ESA Information Centre (HEIC), which was established at ST-ECF, continued to supply material to sec3.qxd 7/15/05 10:01 AM Page 82 82 scientific support activities the media and public. With a unique graphical expression in all lines of products, high scientific quality and innovative distribution methods, the group has received international recognition for their achievements. data flows through sophisticated applications will be deomstrated, along with the use of ‘registries’ to harvest astronomical databases. On a yearly basis, HEIC receives more than 1000 requests from press, public, educators, scientists and others for printed products, information and electronic products. Apart from the production of news and photo releases, innovative educational material, CD-ROMs, brochures and posters, the HEIC has made important contributions. With up to 16 million hits/month, more than 125 000 individual visitors and up to 2 TB of data delivered, the http://www.spacetelescope.org website belongs in the top group of astronomical outreach web sites. Production of PR images from raw data continues. This work has been based on HST data, but also images from ESA missions such as ISO, XMM-Newton and Integral, as well as the ESO VLT and others, have been produced. This work is the most advanced of its kind in Europe, producing high-quality artist’s impressions in 2-D and 3-D using highly optimised, very sophisticated software and hardware technique. High-quality video material for news releases can be produced on timescales of a few days. The online distribution of broadcastquality video material enables broadcasters to use the HEIC material in the evening news on the same day. 3.5.5 HST operational status Slitless spectroscopy from space is competitive with ground-based spectroscopy with large telescopes in those spectral regions where the atmospheric background is high. HST has exploited this advantage and offers slitless spectroscopy facilities on NICMOS and ACS. The ECF has developed expertise in all aspects of slitless spectroscopy through support of the HST slitless spectroscopy modes. Through well-defined agreements with the STScI, the ECF has undertaken full cover for these instruments, from involvement in ground testing, to provision of software to extract wavelength and flux calibrated spectra, to user support. Currently, most effort goes into support for the ACS slitless modes, which cover the red grism for the WFC and HRC, a near-UV prism for HRC and two prisms for the far-UV SBC. The Virtual Observatory (VO) project is evolving quickly. The current ECF archive development includes the creation of a database layer to host ancillary information (metadata, which fully describe the HST products through VO-compliant interfaces), and a database of instrumental characteristics (initially for ACS and WFPC2). The next VO science demonstration is scheduled for January 2005 at ESAC. The VO project is driven by its strategy of regular scientific demonstrations of VO technology, held on an annual basis. The next, based on input from the Science Working Group, will revolve around two science cases: ‘Rich Clusters of Galaxies’ and ‘Asymptotic Giant Branch to Planetary Nebulae Transition’. On the technical side, the use of powerful, distributed workflow processes driving The HST spacecraft is operating nominally, but 2004 saw the demise of STIS on 3 August. To make up for the loss of scientific programmes, an additional 45 proposals have been approved. These had already been rankordered by the original Cycle 13 TAC. A number of already-approved programmes that originally used STIS are in the process of being converted to use other instrument modes, most notably ACS/SBC. RSSD institute staff were actively involved in these complex replanning issues. As the observatory ages, and in the event it has to operate with only two gyros before a refurbishment can take place, preparations and development for the Two-Gyro Science Mode continue, involving a number of the RSSD division staff. Extensive documentation and user information is available at the STScI website, including a Two-Gyro Handbook and a ‘movie’ showing target availability under the somewhat more restrictive scheduling opportunities with two gyros. Detailed simulations show that the impact on image quality from jitter is substantially less than originally assumed, so that a voluntary entry into Two-Gyro Mode is now being discussed in order to preserve the lifetime of the currently operating four gyros. In support of this decision, detailed studies are under way to determine how many orbits per week can be scheduled in two-gyro mode as compared to using three units. On-orbit tests are planned for February 2005. sec3.qxd 7/15/05 10:01 AM Page 83 scientific support activities 3.6 Science Operations and Data Systems Division 3.6.1 Introduction and overview The Science Operations and Data Systems Division (SCI-SD) is responsible for the development and execution of science operations for astronomy missions. After completion of the in-orbit commissioning phase, the Division becomes responsible for overall project management: a Mission Manager is put in overall charge and must ensure that operations are performed in the most efficient manner possible within the constraints; the Project Scientist remains responsible for ensuring maximum scientific return. The Division also provides support in data systems to the entire Department and has long-term responsibility for the science archives of the Directorate. The staff of the Division is located at ESAC and ESTEC. During much of the reporting period, there was also one staff member collocated with the Integral Science Data Centre in Versoix (CH). 3.6.2 ISO The Infrared Space Observatory (ISO) was the world’s first true orbiting IR observatory. With a pointing accuracy at the arcsec level and four highly sophisticated scientific instruments, ISO explored the Universe at wavelengths of 2.5-240 µm with unprecedented sensitivity and capabilities. During its highly-successful in-orbit operational phase from November 1995 to April 1998, ISO made some 30 000 individual scientific observations of all types of astronomical objects. All the data are available to the community via the ISO Data Archive – follow the links from the ISO home page at http://www.iso.vilspa.esa.es. The ISO project is well into its Active Archive Phase, which will run until December 2006. This final phase is designed to maximise the scientific exploitation of ISO’s extensive IR database and to leave behind a homogeneous archive with refined data products, as a legacy to future generations of astronomers. RSSD has the cradle-to-grave responsibility for ISO scientific operations and, from the end of the commissioning phase, overall responsibility for the project. The Division has a team of staff and contractors, led by the Project Scientist, in ESAC. Activities of this team include maintaining the central data archive, providing expert support to the community across all instruments, and coordinating activities with the various national ISO centres. Archive maintenance and improvement activities have continued. Version 6 of the ISO Data Archive, released in July 2003, upgraded the functionality associated with, and visibility of, the Highly Processed Data Products (the result of dedicated projects focused on cleaning the 83 pipeline products from residual instrumental artefacts). Dedicated projects were undertaken, mainly in collaboration with the national centres, to reprocess observations of selected observing modes. As of October 2004, the archive includes 19 such data sets, some also obtained from the community, equivalent to 18% of the archive scientific content. For version 7, released in June 2004, a new approach was defined in the assessment of the data quality, upgrading from a small set of technical quality flags to a well-structured quality report, based on a total of 85 flags. The astronomical community continues to use the ISO archive intensively. There are now 1600 registered users and new users are still registering at a rate of about 10-15 per month. In the first 6 years of use, the equivalent of nearly nine times the total number of scientific observations in the archive has been downloaded, an average monthly retrieval rate of around 13%. Another major activity has been the integration of the ISO archive into the Virtual Observatory. The ISO archive already incorporated many elements of interoperability with other popular astronomical archives. The ad hoc implementation of these functionalities has evolved into a system complying with the new standards set by the VO international community. ISO was one of the first archives to be part of the European VO prototype, as demonstrated in January 2004. Documentation has also been a focus of activity. The legacy version of the five-volume ISO handbook, the definitive standalone guide to the ISO mission and to its data products, was published in early 2004 (as ESA SP-1262) and distributed to the PIs of the ISO observing proposals and to some 300 astronomical libraries worldwide. The proceedings of two recent conferences organised by the ISO Data Centre were also released in the period, Exploiting the ISO Data Archive – Infrared Astronomy in the Internet Age (SP-511) and The Calibration Legacy of the ISO Mission (SP-481). The ISO Active Archive Phase Mid-Term Review was held in June 2004. The Board, composed of external data providers and users, was impressed with the achievements of the ESA and National Data Centres over the previous 2.5 years. Their recommendations focused on making ISO data and results as widely available as possible, by (i) concentrating the activities during the remaining 30 months on maximising the content and visibility of the Highly Processed Data Products, (ii) continuing with the integration of the ISO archive into the VOs, (iii) ensuring prompt publication of the planned special issue of ISO Space Science Reviews, a 400-page book reviewing the results of ISO. In the 2003-2004 period, around 250 papers based on ISO appeared in the major refereed journals (1160 papers are known in total and tracked in the ISO data archive). http://www.iso.vilspa.esa.es sec3.qxd 7/15/05 10:01 AM Page 84 84 scientific support activities With the ISO data archive having establishing itself as a general astronomical research resource and as an important tool for planning future missions, with activities continuing on enhancing its contents and functionality, many more astronomical surprises and discoveries from ISO are still expected. 3.6.3 XMM-Newton XMM-Newton is an X-ray astrophysics observatory, launched on 10 December 1999 with a projected and designed lifetime of over 10 years. It enables astronomers to conduct sensitive X-ray spectroscopic observations of a wide variety of cosmic sources. It is specifically designed to investigate in detail the spectra of cosmic X-ray sources down to a limiting flux of 10–15 ergs/cm2/s. It is able to detect X-ray sources down to a few times 10–16 ergs/cm2/s; however source confusion starts to play a role at these flux levels. The principal characteristics of XMM-Newton, with its three telescopes and suite of complementary instruments (EPIC, RGS, OM used simultaneously), can be summarised as follows: — effective aperture of 4500 cm2 at 1 keV (12.4 Å) and 1000 cm2 at 10 keV (1.24 Å); — almost constant angular resolution across the full waveband of ~15 arcsec HEW; — X-ray field of view ~30 arcmin; — capability of performing sensitive mediumresolution spectroscopy with resolving powers 100700 over the wavelength band 5-35 Å (3502500 eV); — broadband imaging spectroscopy from 300 eV to 12 keV (1-40 Å); — simultaneous sensitive coverage of the wavelength band 1600-6000 Å (~17 arcmin FOV) through a dedicated optical monitor, co-aligned with the X-ray telescopes; — continuous coverage of a source for up to 42 h. Further details, including access to the data archive, may be found by visiting http://xmm.vilspa.esa.es. The Division has overall management responsibility for the project and is directly responsible for the execution of science operations. Mission operations for XMMNewton are conducted from ESOC, while science operations are conducted from ESAC, where the Science Operations Centre is located. The main tasks of the SOC are: — monitoring payload operations in real time; — performing mission planning and constructing an optimally efficient schedule. This includes issuing and processing announcements of opportunity; — maintaining and updating all XMM-Newton handbooks; http://xmm.vilspa.esa.es/ Figure 3.6.3/1: These four images illustrate the XMM-Newton observtion of GRB 031203. The ring structures expanding around the point source are the first time-dependent light echo seen in X-rays. — tracking the maintenance and implementation of change requests to the SOC operations subsystems by external contractors; — defining, implementing and tracking procedures for operating the scientific instruments; — implementing instrument calibration observations, coordinating and participating in their analysis, and delivering finalised calibration files to the community; — co-developing, pre-release checking and distributing the Science Analysis Software (SAS) and the associated data products. During the reporting period, the work still performed at ESTEC (except for mission management) was transferred to ESAC. During Autumn 2003, the Division prepared the case for extending mission operations and presented it to the scientific advisory structure and to the SPC, which unanimously approved the principle of an extended mission up to 31 March 2008. With such an outlook, efforts to streamline and reduce the cost of operations continue. In this context, a reduction in (contractor) staff has already been implemented without affecting the overall performance of the observatory or the ground segment. One of the other elements to ensure that an extended, cost-effective future is possible has been the decision to transfer the operating system for the mission control systems from SCOS-1b to SCOS-2000. This activity is nearing completion and will, inter alia, provide a solid operating environment up to the end of the mission. sec3.qxd 7/15/05 10:01 AM Page 85 scientific support activities A new general management structure for satellites in orbit was introduced. For XMM-Newton, this meant a separation of the role of Mission Manager and Project Scientist. The Mission Manager continued to work 50% on XMM-Newton and a new Project Scientist was appointed at ESAC. This new set-up is working extremely well. 85 scheme has been running for almost a year now and is under evaluation. There is a clear indication of increased science output from the SOC team contributing to the 650 refereed XMM-Newton publications so far. 3.6.4 Integral The XMM-Newton users’ group now meets on an annual basis, instead of biannually, as it was felt the mission is now routinely and reliably turning out all products expected by the community. In general, it is very positive about the status of the mission. With the improved knowledge and experience both in mission planning and schedule execution, the SOC can now carry out the necessary replanning and get the satellite repointed in response to a target of opportunity alert in as little as 4 h 40 min after receipt of the alert. This is well beyond what the mission was designed for, and provides spectacular science results (Fig. 3.6.3/1). The calls for observing proposals are now issued annually by the SOC and the process has become routine. The uptake by the community remains very high, with 692 proposals submitted in response to AO-3 and 657 in response to AO-4. The oversubscription factor is around 5-6. There is a clear and continuing trend to go for longer observations and multiple sources per proposal. A number of new releases of the XMM-Newton Science Archive (XSA) and the Science Analysis Software (SAS) were made available to the community. The XSA has now become the standard tool for the community for retrieving (and searching) both proprietary and public data. A few thousand public data sets are available through the XSA. One of the major new components integrated into the XSA was the first XMM-Newton source catalogue (1XMM), generated by the Survey Science Consortium (SSC, PI: M. Watson, Leicester, UK). Preparations for generating a second, extended, source catalogue have started inside the SSC, and ESAC is actively regenerating data sets wherever new processing (attitude, timing, etc.) provide improvements. The SAS (now at release 6.0) has become the de facto standard for analysing XMMNewton data; it is a complete suite of tools, which now contains the tools to analyse grism spectra from the Optical Monitor. The observatory has implemented support of COSPAR regional education activities (New Delhi, 2003; Durban, 2004) and is routinely organising workshops at ESAC to teach people how to use the XMM-Newton data analysis system. In order to support observatory staff in executing their science research objectives, the concept of a ‘science day’ has been introduced. This is a fixed day in the week that is set aside for research. On this day, in principle, no meetings or other functional duties are scheduled. The The Integral gamma-ray observatory is dedicated to spectroscopy and imaging of celestial gamma-ray sources in the energy range from 15 keV to 10 MeV. It was launched on 17 October 2002 by a Russian Proton rocket. The payload consists of two imaging gamma-ray instruments, one optimised for spectroscopy (SPI) and one for high-resolution imaging (IBIS). These are supported by co-aligned X-ray (JEM-X) and optical (OMC) monitors. All three high-energy instruments use coded masks for imaging. Further information is available at http://astro.estec.esa.nl/Integral. The majority of Integral observing time is available to the general astronomical community via calls for proposals, with a smaller amount (currently 25%) used for survey-type Core Programme activities such as deep exposures of the galactic centre region and regular scans along the galactic plane. Integral operations continue smoothly, with the spacecraft, instruments and ground segment performing well. A major milestone was reached on 17 July 2004 when the first Integral observations entered the public domain. These are available to the scientific community via the on-line archive at the Integral Science Data Centre. The Division has overall management responsibility for the project and is directly responsible for the Integral Science Operations Centre, handling uplink and coordination activities. During the reporting period, ISOC was located at ESTEC but is being moved to ESAC. Downlink science operations (data processing and distribution) are the responsibility of the Integral Science Data Centre (ISDC, Versoix, CH). Mission operations are conducted from ESOC. The main tasks of ISOC are: — to issue Calls for Observing Proposals and to process the submitted proposals; — to conduct the scientific mission planning, including processing ToO requests; — to operate, jointly with the ISDC, a web-based helpdesk to support Integral users who have questions about any aspect of the mission, or their own observations. Additionally, in close collaboration with the Integral Science Working Team, the ISOC works: — to finalise the Core Programme of guaranteed-time observations for each AO-cycle and implement them into the ISOC scheduling system; — to prepare and manage the instrument in-flight calibration during the nominal and extended mission phases; http://integral.esac.esa.int sec3.qxd 7/15/05 10:01 AM Page 86 86 scientific support activities creation of the corresponding commands to be sent to the spacecraft. The Integral observing schedules, both shortterm and long-term, are available on the web. The overall observing programme is summarised in the exposure map (Fig. 3.6.4/1), which includes all observations to February 2005. Figure 3.6.4/1: Integral exposure map covering scientific observations from December 2002 (start of the nominal mission phase) until February 2005 (end of AO-2 observing programme). — to support the instrument teams in instrument configuration and operations (e.g. telemetry allocation, annealing of the SPI detector unit). During Autumn 2003, the Division prepared the case for extending mission operations and presented it to the scientific advisory structure and to the SPC, which unanimously approved the principle of an extended mission up to 31 December 2008, with a review of the science foreseen in Autumn 2006. An element of the mission extension is to move ISOC from ESTEC to ESAC in order to increase synergy with XMM-Newton. The Mission Manager is ensuring that this transition is conducted in the most cost-effective way, while maintaining full operational capabilities. A plan for the evolution of the ISOC manpower has been developed by the ISOC manager and the activities defined in the plan are underway, with science operations transferring from ESTEC to ESAC in February 2005. During the reporting period, two Calls for Observing Proposals (AO-2 in 2003, AO-3 in 2004) were issued and processed. The response from the community remained strong, with 142 and 108 proposals received, respectively, with over-subscription factors of 8 for AO-2 and 4 (equivalent to 6 if the duration of the AO is taken into account) for AO-3. After each AO, the pointing directions of the approved observations are scanned by ISOC staff for targets close together in the sky which can be observed in a single pointing – hence saving observing time through amalgamation of several independent research proposals. This is particularly important for Integral where the observations are, owing to the low fluxes, generally long, but the fields of view of the gamma-ray instruments are very large (the fully coded fields of view are 16º for SPI and (9x9)º for IBIS). The accepted proposals are processed at the ISOC into an optimised observing plan consisting of a timeline of target positions, together with the corresponding instrument configurations. These are then forwarded to the Mission Operations Centre (MOC) at ESOC for the The gamma-ray sky is highly variable and interesting new targets can, and do, appear unexpectedly anywhere in the sky. When this happens, a ‘Target of Opportunity’ (ToO) request may be made. The Project Scientist, supported by the ISOC mission planners, evaluates the request and decides on the basis of scientific merit and on the impact of the rescheduling, whether to go ahead. If the request is granted, the ISOC generates a new observing programme for the interval concerned and, inter alia, makes this available on the WWW to aid astronomers planning coordinated observations. During the reporting period, 36 requests for ToO follow-up observations were received, out of which 16 were accepted and successfully observed. The achieved sensitivities of the Integral high-energy instruments are now close to the statistical limits derived from the background counting rates and effective areas. The Mission Manager has coordinated the activities to improve the achieved sensitivities through better observing techniques, background modelling and analysis software. One of the few major payload anomalies has been the loss of two of the 19 SPI detectors. Both of these losses followed annealing, when the SPI detectors are ‘baked’ to recover the loss of energy resolution caused by radiation damage. The Mission Manager has coordinated the efforts to understand the failures, using both in-flight tests, ground tests on flight spare hardware, and computer modelling. Once the failures are understood, it will be possible to decide on future annealing strategies. The Project Scientist coorganised the 5th Integral Workshop (Munich, February 2004) and co-edited the proceedings (SP-552). Support is being provided to organise an Integral workshop in January 2005 (ESTEC) and the 6th Integral Workshop in 2006 in St. Petersburg (Russia). Finally the Project Scientist, in coordination with the ISWT, contributed to the definition of the terms of reference for the new Integral Users Group and the associated update of responsibilities for the ISWT as laid down in the Science Management Plan. 3.6.5 Astro-F Astro-F is a Japanese mission with the prime goal of making a second-generation all-sky IR survey with higher sensitivity and longer wavelength coverage than IRAS. ESA is collaborating with JAXA to provide sec3.qxd 7/15/05 10:01 AM Page 87 scientific support activities 87 tracking support (use of a second ground station) and assistance with the survey data reduction (pointing reconstruction) in return for 10% of the observing opportunities during the non-survey parts of the mission, to distribute to the ESA community. The SPC approved this collaboration in Autumn 2000. During the reporting period, JAXA/ISAS have announced launch delays from February 2004 to end-2005 or early 2006. The Division has overall responsibility for all of ESA’s contribution to this mission. Implementation of tracking support has been delegated to ESOC, who, during the reporting period, have designed, implemented and tested the various upgrades and customisations necessary to enable the Kiruna tracking station to provide the required service. All equipment is now in hibernation until launch preparations start 6 months before launch. Activities for pointing reconstruction and community support are carried out by the Division’s team in ESAC. Work on the input reference catalogues, needed for the pointing reconstruction task, was completed as planned by end-2004. The Pointing Reconstruction User Requirement Document has been issued and the detailed software design is underway. Planning for the European Call for Proposals is based on issuing the call in the May-June 2005 timeframe, preceded by a call for letters of intent, once the launch date has been finalised. 3.6.6 Herschel Science Centre development The science ground segment of the Herschel Space Observatory (Section 3.1.2) is being implemented as a distributed architecture with the science community being supported by an ESA-provided Herschel Science Centre located at ESAC (US astronomers supported by the NASA Herschel Science Center at IPAC, Caltech) and instrument operations being carried out from three Instrument Control Centres, located on the PIs’ premises. The key software ‘glue’ holding these centres together is the Herschel Common Science System (HCSS), being built jointly by the above parties, under the leadership of the Division’s Herschel Science Centre Development Team. Within RSSD, the Astrophysics Missions Division has overall responsibility for the scientific integrity of the mission, while the Science Operations and Data Systems Division is responsible for implementing the science operations in close collaboration with the instrument teams. From the end of the in-orbit commissioning phase, the latter Division will take over overall project management responsibility. The HCSS is an ensemble of services supplied in the form of a single, coherent and mostly platformindependent software system. Its users include the Herschel Science Centre, the Instrument Control Figure 3.6.6/1: A month-by-month history of HCSS software problem reports (SPRs) and software change requests (SCRs) and the change in the number of open SPRs/SCRs (pink line). Centres, and observers using Herschel. Seen end-to-end, these services include support for (i) proposal submission, (ii) proposal evaluation, (iii) helpdesk support, (iv) generation of observing schedules compliant with the interfaces agreed with the Mission Operations Centre, (v) reception and archiving of telemetry, (vi) instrument data processing software, (vii) data products in the Herschel archive. One of the top-level requirements driving HCSS development is that it supports the concept of smooth transition, in which a nucleus of the system that is to be used for in-flight operations already supports InstrumentLevel Tests in the laboratories of the PI teams several years before launch. Owing to this requirement, HCSS development started in early 2000. During the 2003-2004 reporting period, seven releases were made, emphasising the consolidation of the development and the software having matured from the early prototypes into production-level code. The status of the development is: — the system is in daily use for Instrument-Level Tests of the Avionics/Cryogenic Qualification Models in the PI laboratories; — the system has been integrated into the Instrument EGSE for use in satellite-level tests; — significant progress has been made in the development of a Herschel Interactive Analysis framework, with a group of scientific end-users giving direction to and providing priorities for this resource-limited development; — development of the next system release, which will support submission and handling of Herschel sec3.qxd 7/15/05 10:01 AM Page 88 88 scientific support activities observing proposals and a first implementation of the scientific mission planning system, is well under way for delivery in 2005. Examining the trends of the software problem reports (SPRs) and software change requests (SCRs) handled by the HCSS Configuration Control Board gives a vivid insight into the development of the system (Fig. 3.6.6/1). Initially, until the end of third-quarter 2003, there was a steady but slow trickle of inputs. Then, a steady rise started as both the number of users at the PI institutes and also the intensity of their use increased. In addition to the increase in average flow, the submission rate shows rather pronounced peaks, well correlated with dates of user releases of the system. This indicates that the system tests performed by the developers and acceptance tests performed by the users do indeed detect software problems that are not encountered during normal use of the system. Note also that the difference in open SPRs/ SCRs from one month to the next remains almost constant despite the monthly influx, showing that the HCSS developers just about manage to keep up. 3.6.7 Information technology support activities The Division provides support in data systems to the entire Department. The focus is on consolidating and optimising the various services with the needs of the community, the cost-effectiveness of the infrastructure and the requirements of remote users kept firmly in mind. The Department’s highly valued technical mail service allows ease of e-mail access to the peripatetic staff. The mail service is closely integrated with the LDAP (Lightweight Directory Access Protocol) services set-up on which is built the RSSD intranet. By sharing common resources, we have created a virtual community of all the RSSD outstations. The RSSD web portal has been developed to offer secure Single-Sign-On access to shared services, including contact and personal information, documents, web-page creation and maintenance, mailing lists, directory services, mailing labels, publication lists, etc. in the case of Rosetta, a valuable Knowledge Base to take forward through the long mission. Tools have been created to harmonise the working methods; these include the Publication Data Base, a tool for registering and approving the publications of staff members. This tool is integrated with the web services such that an accepted paper is available to the public on line. The same database may be used, in connection with the developed Hermes community contact system, to distribute electronically (or by paper if no e-mail address is available) staffs’ preprints, with the resulting saving in secretarial effort, printing and postal charges. The various RSSD web sites have been consolidated into a unified RSSD site at http://www.rssd.esa.int. Here, all the information needed by end users of a science mission may be posted with the necessary protection of proprietary data and personal information. All project scientists have access to a tool for developing their web pages; it is optimally designed for us using PHP methods and My_SQL database. Although the site is not completely finished, it means we have significantly reduced the maintenance overhead for the web sites, freeing up Project Scientist time. The departmental computing architecture is SUN-Solaris based – a highly reliable architecture. During the reporting period, numerous obsolete items have been replaced by a small number of modern powerful file servers, with obvious economic benefits in performance and maintenance. Where appropriate, Linux machines have been introduced, keeping in step with the academic community’s tendency towards Linux. Windows is both the Agency’s and the general public’s preferred platform and the Solaris team has developed a close working relationship with the Windows support team. Interoperability is the keyword and facilities are shared among the office, laboratory, science, operations and research users, such as software licences, storage and printers. 3.6.8 Archive and Virtual Observatory activities These elements make up a software tool-box that enables the establishment of virtual communities, not just for RSSD at large but also the external project teams spread around the world. Such virtual communities have already been set up for Planck, Gaia and Huygens, and it is expected that, with management support, more projects will soon adopt this technology. The Science Archives Group at ESAC has been consolidated to provide horizontal support for archive activities to many science projects, ranging from astronomical missions to planetary missions. Development and maintenance of the various archives is done in an efficient and cost-effective manner by using common architecture, code and manpower. This is demonstrated by the achievements of the group during the reporting period, including: The Department’s documents are centrally managed using the Document Management system (based on Livelink). This permits staff to access their assets (document libraries) while on the road, publish documents directly to the web and create, as for example — the ISO Data Archive allows ingestion and access to highly processed data products provided by expert user groups, and now provides a more detailed quality report for each ISO observation; — the XMM-Newton Science Archive now includes sec3.qxd 7/15/05 10:01 AM Page 89 scientific support activities 89 powerful and friendly access to the XMM-Newton point source catalogue as well as on-the-fly processing capabilities to offer users the most up-todate data products; — a mirror of the Integral Science Data Archive, together with an updated user interface based on those built for ISO and XMM-Newton, has been developed to support calibration and monitoring activities within ESA, offering powerful query and automatic data distribution systems; — work has started on the Herschel Archive Browser for instrument-level and system-level test data. 3.7 Experience gained in the astronomy archives has been reused to develop the Planetary Science Archive (PSA). This will be the single portal to all ESA planetary missions data. Giotto data have already been ingested; Mars Express, SMART-1 and Rosetta data will be incorporated from early 2005. Huygens, Venus Express and BepiColombo data sets will come in the future. The PSA also offers a data set validation tool to help the PI teams to provide data sets compatible with the PSA/PDS data sets standards. 2003-2004 saw the successful completion of a number of flight hardware activities. After the March 2004 launch of Rosetta, MIDAS, RPC-MIP, OSIRIS and SESAME all successfully underwent their first commissioning. SPEDE on SMART-1 and ASPOC on the two Double Stars are also performing as expected. Activities on the Virtual Observatory (VO) have been expanded in the second year of the reporting period. VOs are defined as a collection of interoperating data archives and software tools that use the Internet to form a scientific research environment in which astronomical research programmes can be conducted. The ISO Data Archive and XMM-Newton Science Archive have already been updated to support existing VO protocols, such as Simple Image and Spectra Access, and are, currently, two of the few VO-compliant astronomy archives worldwide. Following this success, ESA is providing more VO-dedicated manpower in 2005 and 2006 to fully integrate our archives into the VO world, to develop tools to support the VO community, to increase ESA and member-state data centre involvement in worldwide VO activities, and to position ESAC as the Space Astronomy VO centre in Europe. Science Payload and Advanced Concepts Office The Science Payload and Advanced Concepts Office (SCI-A) provides support to the Agency’s science missions and technology programmes as well as the research programme of RSSD. The various sections focus their support in these three important areas as well as being responsible within the Directorate for the assessment of future science missions. 3.7.1 Science Payload Instrument Section (SCI-AI) Two additional flight projects are nearing completion. The first is the COROT Digital Processing Unit. The Engineering Model was delivered to the project and is undergoing integrated tests. The assembly and electrical tests of the flight and flight spare models (three in total) were completed at Astrium GmbH and were in the SCI-A laboratories by December 2004. The second project is the Solar Electron Proton Telescope (SEPT) for the STEREO mission as part of the IMPACT suite of instruments within the Solar Electron Proton package. SEPT consists of two dual, doubleended magnet/foil solid-state detector particle telescopes that cleanly separate and measure electrons in the energy range 20-400 keV and protons of 60-7000 keV, while Figure 3.7.1/1: Top view of the STEREO Flight Model analogue board. sec3.qxd 7/15/05 10:01 AM Page 90 90 scientific support activities Fig. 3.7.1/2 the complete system integrated in its housing with the various detectors. The four SEPT Flight Models (plus one spare) are assembled and have undergone final environmental tests. They were formally delivered to the project in December 2004 after completion of the calibration campaign. Figure 3.7.1/2: The assembled STEREO Flight Model Models. Figure 3.7.1/3 shows the first spectra obtained with the instrument using the electron conversion lines of a 207Bi source. The PDFEs were operated in full anticoincidence mode. The green curve is related to CS1, the centre segment of D1. The red curve shows the fluence observed on CS2, the centre segment of D2. The blue curve is related to XT1, the cross-talk ring of D1. At top right is a basic sketch of the position of the source with respect to the detectors. The K conversion lines are nicely resolved. The different lines are also visible on CS2, shifted by ~110 keV, the average energy deposited by electrons crossing D1. These results indicate that, by focusing on a detailed design, an optimised low-resource instrument can be developed without loss of overall performance. This approach will continue to be developed in SCI-A through the study of Highly Integrated Payload Suites (HIPSs). 3.7.2 Science Missions Section (SCI-AM) The Science Missions Section of SCI-A is responsible for providing support to science missions in orbit, under development and under assessment, and for planning longer-term future mission developments. Figure 3.7.1/3: The first spectra obtained with one of the telescopes and the dedicated electronics, using the electron conversion lines of a Bismuth-207 source. providing anisotropy information through the use of several fields of view. Two SEPT units (NS: North-South direction, E: Ecliptic) are located on each STEREO spacecraft. The electronics were designed and fabricated by SCI-A for RSSD, while the housing and sensors were provided by the University of Kiel (D). The major challenge of SEPT involves the growing need for compact and highly integrated instruments. SEPT is based on the Particle Detector Front End ASIC developed under ESA’s GSTP. With 640 g and 600 mW per unit, the instrument demonstrates the technological development that is possible and which will have to be matured further to respond to future, ever-more demanding space missions. Fig. 3.7.1/1 shows the assembled analogue board and Support to the external scientific community is provided directly and indirectly. Directly, for specific requests related to instrument development, to payload reviews and to programmatic aspects or by performing dedicated studies on the payload complement baselined for future missions. Indirectly, by assessing new missions, thus defining the requirements of future instruments and the related technology development needs, and by supporting missions already under development. As an example, over the last few years, SCI-AM staff have followed the development of the SMART-1 payload units closely, supporting PIs and the Project Scientist throughout the different mission phases, including commissioning after launch and performance verification. In the 2003-2004 period, SCI-AM staff provided technical payload support to both RSSD (SCI-S) and the Science Projects Department (SCI-P) for a number of missions under development, such as Planck and Herschel (participating in project reviews) and Integral (Instrument Final Acceptance Review and In-Flight Performance Review). In 2004 SCI-AM contributed to the Systems Requirements Review of NIRSpec and MIRI, two major instruments provided by ESA to the James Webb Space Telescope. SCI-AM staff also sec3.qxd 7/15/05 10:01 AM Page 91 scientific support activities 91 module, as well as to assess the needs of a mission aimed at investigating the ‘Pioneer effect’ (deviation from the gravitational theory at large distances from the Sun). Another TRS is the Solar Polar Orbiter, a mission exploiting solar sailing and aiming to observe the Sun from very high heliospheric inclinations Figure 3.7.2/1: The Solar Orbiter orbiting the Sun at 0.2 AU during the science mission phase contributed to the Gaia Mid-Term Review (September 2004), providing payload and detector expertise, including integrated support to the Project Scientist in areas such as radiation damage and detector modelling. Considerable support on technical and programmatic areas has been provided for the BepiColombo reassessment and the following AO and payload selection process. As part of its duties, SCI-AM contributed to the cost and risk assessments of several missions (such as BepiColombo, Darwin, Solar Orbiter and the MIRI instrument), including payload, flight and ground segments, with the final goal of estimating the Cost-at-Completion of these future ESA science missions. A major task under the responsibility of SCI-AM during 2003-2004 was the Solar Orbiter assessment study (Fig. 3.7.2/1). Activities included the preparation of all mission reference documents, the conduct of a dedicated industrial study on the payload complement, the completion of two parallel competitive studies at system level, the preliminary mission analysis and mission control study, and a complete mission cost-risk assessment. With such an in-depth study of all these mission elements Solar Orbiter is well placed to move into the development phase in 2006. Technology Reference Studies (TRS) in astrophysics, fundamental physics and solar physics are also being developed by SCI-AM, based on the ideas put forward by the scientific community following the ESA Call for Ideas and the Cosmic Vision workshop that took place in September 2004. SCI-AM staff are performing a preliminary study on a future Gamma-Ray Lens project, as a potential post-Integral mission and targeting photon energies even above 500 keV. Similarly, in fundamental physics, work is under way to assess requirements for a standard fundamental physics payload and spacecraft SCI-AM staff are responsible for the Darwin Groundbased Nulling Interferometer Experiment (GENIE) definition phase, which involves conducting two industrial parallel competitive studies to establish the feasibility, performance, preliminary design and cost. GENIE may be installed at the VLT of ESO (Chile) as a precursor to the future Darwin payload. GENIE has a two-fold objective: to exercise, on the ground, nulling interferometry in prospect of the Darwin mission; to provide the scientific community with a sophisticated instrument capable of obtaining valuable scientific data. The industrial studies ran during 2004 and the definition study will be completed at the end of March 2005. Finally, SCI-AM personnel supported a number of space science instruments being studied or developed for the ISS. Examples of instruments under study are EUSO and Lobster. Support to the instrument team has been provided in the case of SolACES, a UV radiometer under development. 3.7.3 Planetary Exploration Studies Section (SCI-AP) The principal effort of the section has been the execution of the 9-month reassessment of the BepiColombo mission to Mercury, with the aim of maximising the scientific performance and optimising the payload complement, while reducing costs and programmatic risk. The change of the mission profile from a split launch for MMO and MPO into a single SoyuzFregat 2B launch brought a major reduction in cost. Coupled with a detailed cost and risk assessment, this has allowed the mission to move into the definition and development phases. The section now provides support to the Project Scientist and project team in such areas as payload architecture, and participated, in particular, in the evaluation of instrument proposals after the Request for Proposals in support of the Payload Review Committee. The section provides support to a number of planetary missions such as Venus Express, where the external magnetometer team was supported during qualification of the instrument and its boom. In the case of Rosetta’s MIDAS, a major effort went into the final design, integration, testing and verification of the flight instrument and flight spare. Commissioning of MIDAS after launch was successfully performed by SCI-AP personnel in collaboration with the PI team. Parallel activities, supported by SCI-AI, are establishing a sec3.qxd 7/15/05 10:01 AM Page 92 92 scientific support activities Figure 3.7.3/1: The Europa Mini-Satellite Orbiter with its ice-penetrating radar deployed. The lifetime is about 60 days after entering polar orbit, sufficient for two complete high-resolution mappings of the surface. reference database to determine the magnetic properties of selected meteorites and prepare for the data return. Support has been provided on specific instruments for Solar System research to the Instrumentation Section SCI-AI. For example, the ASIC development for STERO and the major contribution to the development of the DSP-based DPU for COROT, based on the experience with the DPU of Rosetta’s OSIRIS. Finally, in preparation for future technology planning as well as for establishing potential feasible mission scenarios at an early phase, the section has been prominent in running a TRS series related to Solar System science. These have included the following toplevel mission profiles: — exploration of the Jovian system and specifically the mapping of Europa using a series of mini-satellites (Fig. 3.7.3/1); — in situ exploration of Venus via an aerobot coupled with a series of microprobes; — a mini-satellite sample and return mission to the Martian moon Deimos; — a solar polar microsat orbiter using a solar sail to raise the ecliptic inclination to 90º; — a microsat to explore the boundary of the heliosphere, heliopause and beyond through the use of a large solar sail to achieve initial high velocities (Fig. 3.7.3/2). Such mission studies allow the section to contribute Figure 3.7.3/2: The Interstellar Heliopause Probe (IHP) with its high-gain antenna, RTGs and boom system (top), and the conceptual design showing the instruments’ field of views (bottom). The sail would be shed at about 5 AU since no further major gain in acceleration could be achieved. The science phase would then begin using the plasma instruments. The probe would reach the assumed heliopause (~200 AU) in about 25 years. meaningful technical data to the future technology plans, as well as providing quantitative data for the future science programme through the Cosmic Vision process. 3.7.4 Advanced Technology Section (SCI-AT) The Advanced Technologies Section provides support to the community in two ways: by developing basic enabling technologies for future missions and instruments, and by offering specific technology support to on-going activities or studies. The key areas are in the technologies required for science payloads and, in particular, in advanced optics and detectors. It is sec3.qxd 7/15/05 10:01 AM Page 93 scientific support activities 93 systems should be possible without recourse to the very low temperatures required for current sensors based on superconductors. Finally, the section’s technology expertise has been used to support ESA missions past and future including: Figure 3.7.4/1: The Wolter 1 micro-channel plate optics developed as a prototype a variant of which will form part of the imaging X-ray spectrometer instrument on the BepiColombo mission. particularly considered that precision lightweight optics will be a crucial enabling technology, allowing lowercost missions with much higher sensitivities. Specific areas of development include lightweight X-ray optics such as those based on glass microchannel plates (Fig. 3.7.4/1) and silicon micro-pore optics. These technologies have been studied in detail for future mission applications such as Lobster, a wide-field X-ray telescope, the X-ray surface fluorescence spectrometer on BepiColombo, and the XEUS large effective area X-ray mirror. In the case of XEUS, the section is also handling all mission-related aspects, including payload accommodation, system engineering, mission analysis and mission profile optimisation, because the optics technology drives all other issues. At a later stage, the mission will be transferred to SCI-AM for further mission development at system level. In addition to these specific soft X-ray optics technologies, optics requirements for the hard X-ray and gamma-ray regions are under active study or development, and preliminary studies of the needs at far-IR wavelengths have begun. Essentially, the experience gained in the development and deployment of low-resource optics at X-ray wavelengths for astrophysics and planetary missions will migrate across to other wavelengths and disciplines. The second area of key expertise is in advanced detector technologies, which have been studied and developed over a wide range of wavelengths. A programme for the development of solid-state neutron detectors for planetary science has also been introduced. Of particular note is the study of low band-gap semiconductors for the EUV and soft X-ray domains, where photon-counting — XMM-Newton in-flight instrument calibration; — radiation damage annealing studies on Integral; — radiation damage analysis for Gaia and BepiColombo; — BepiColombo spectrometers and particle monitor design; — supporting the development of specific payload technologies for BepiColombo; — CCD design and systems analysis for the Eddington focal plane camera; — establishing the Solar Orbiter Technology Development Plan; — system design studies for XEUS instruments and mirrors; — developing the XEUS micro-pore mirror; — supporting the Darwin Technology Development. 3.7.5 Darwin special project group Darwin, the near-IR nulling interferometer, is a special project under study in SCI-A. This mission requires multiple spacecraft to fly in formation at L2. The mission objectives are to detect and determine the nature of extrasolar terrestrial planets out to a distance of about 25 pc. This is achieved through nulling interferometry at 6-20 µm. The Darwin special project group has concentrated on studying in detail the optical architecture of the mission with the aim of maximising the scientific return while controlling the cost, complexity and risk. This has been achieved through the use of four spacecraft: three identical spacecraft carry ~3 mdiameter mirrors pointed at the target star, while a fourth spacecraft combines the three transferred beams under accurate phase control, including achromatic phase shifts. In this way, the light from the central on-axis star can be effectively reduced by six orders of magnitude while the transmission map has off-axis regions close to the star, where terrestrial planets would be detectable depending on the planet’s orbital period and observation time. Rotation of the constellation coupled with multiple observations would allow planets to be detected and their orbital periods to be established. Longer observations of any planet, once detected, would allow its atmosphere to be characterised through broadband spectroscopy. The Darwin team has been able to reduce the mission complexity, and thereby its cost, by introducing a novel way of beam combination. This technique is based on multi-axial beam injection into a single mode waveguide. Recognising that the waveguide injection losses would also occur when using traditional beam combination sec3.qxd 7/15/05 10:01 AM Page 94 94 techniques, such as beam splitter plates, where a waveguide would be used for wavefront filtering, and that the technique allows odd numbers of beam to be efficiently combined, the team determined that an efficient nulling interferometer, involving the minimum number of beams, could be realised. The concept has been developed and now forms the mission baseline. An initial laboratory verification of the concept has been completed and will be complemented by more refined breadboards. The team continues its studies in nulling interferometry by pursuing explorative work in system design and modelling. It is envisaged to place the four spacecraft in orbit around L2 using a pair of Soyuz-Fregat launchers. The cruise duration to L2 is of the order 100 days. The Darwin team is looking further into the details of the payload and its accommodation, together with the development of the mission at the system level. scientific support activities sec3.qxd 7/15/05 10:01 AM Page 95 symposia and workshops 95 4. OTHER ACTIVITIES 4.1 Symposia and Workshops organised by RSSD The proceedings were published in Nucl. Phys. B (Proc. Suppl.) 132 (2004). 4th Cluster Workshop ‘1st Cluster Tail Workshop’, Graz, Austria, 26-28 March 2003 About 60 people attended this workshop to discuss the structure and dymanics of the Earth’s magnetotail. A key topic was thin current sheets that are unstable to magnetic reconnection processes that energise charged particles, causing fast plasma flows and magnetic flux ropes. These events lead to precipitation of particles into the Earth’s atmosphere, triggering auroral displays. ‘2nd Eddington Workshop: Stellar Structure and Habitable Planet Finding’, Palermo, Italy, 9-11 April 2003 While the programme of this workshop focused on some specific aspects of the preparation of the Eddington mission (the choice of planet-finding field and the data processing approach), broad science topics in the fields of planet-finding and asteroseismology were also extensively covered. The workshop was attended by 150 scientists from most ESA Member States as well as Canada, USA, Australia, Hungary and the Czech Republic. One of the workshop’s key issues was the selection of the region of the sky where Eddington would have searched for habitable planets. The workshop generated a broad interest in the media, resulting in coverage in national newspapers in Italy as well as national TV and radio coverage in some of ESA’s Member States. ‘The Restless High Energy Universe’, Amsterdam, The Netherlands, 5-8 May 2003 About 140 people attended this conference dedicated to results from the BeppoSAX mission. The Italian-Dutch X-ray astronomy satellite was launched in April 1996 and operated for 6 years. It revolutionised the study of gamma-ray bursts (GRBs) by discovering long-lived X-ray afterglows which, at long last, allowed the redshifts of GRBs to be determined and confirmed their cosmological distances. During the conference, these results and their legacy were reviewed together with BeppoSAX results on clusters of galaxies and supernova remnants, active galactic nuclei and the X-ray background, stellar-mass black holes and neutron stars. It is clear that results from the broadband (0.1-300 keV) instrumentation on BeppoSAX played major roles in many areas of high-energy astronomy. The workshop also examined the legacy of the mission, showing how discoveries from the mission have helped to define the scientific priorities of later missions such as Swift and Integral. ‘5th Cluster Workshop’, Orleans, France, 12-16 May 2003 This workshop dealt with spatio-temporal analysis and multi-point measurements with Cluster. About 100 participants attended, and the main topics were the dayside plasma boundaries of the magnetosphere and the local characterisation of the space plasma. The magnetic reconnection that also occurs on the dayside magnetopause was widely discussed: here the reconnection causes the transport of energy, momentum and particles from the solar wind into the magnetosphere. The measurement of electric current was also discussed: the measurement is based on Ampere’s Law and requires four satellites that are properly separated in order to derive the current flowing across the satellite constellation. ‘New Perspectives for Post-Herschel Far Infrared Astronomy from Space’, Madrid, Spain, 1-4 September 2003 With Herschel and its instruments well into their development and construction phase, it was timely to discuss the long-term future of far-IR space astronomy and to design a development plan for the post Herschel era. ESA has already created a framework plan (Cosmic Vision) for future missions based upon discussions and considerations from the Horizon 2000+ planning exercise. However, these activities took place some time ago, when ISO was beginning operations and before the implementation of Herschel got underway. More recently, in 2002, US astronomers considered the options for future far-IR/sub-mm space astronomy and have constructed a roadmap for technology and mission development. At this meeting, about 75 members of the European (far-)IR astronomical community (both scientists and instrumentalists) met to discuss the long-term scientific goals requiring observations in space in the 50-600 µm range, to review the instrumentation capabilities to be developed and to discuss a strategy for implementation. ‘IAA/ESA Workshop on the Next Steps in Exploring Deep Space’, ESTEC, 22-23 September 2003 This workshop, organised by ESA and the IAA, was attended by more than 125 participants. It built on an ongoing IAA cosmic study ‘Next Steps in Exploring Deep Space’ in order to give a vision for the exploration sec3.qxd 7/15/05 10:01 AM Page 96 96 of space by humans in the first half of the 21st century. The purpose was to provide a roadmap for a systematic, logical and science-enabled plan for exploration of the Solar System and observation of the Universe, a programme to gradually but systematically establish a permanent presence and infrastructure at each outpost along the way. The workshop considered prorities established by various communities and space agencies across the world, and discussed the spaceflight infrastructure required to pursue these goals, including the relevant policy, international aspects and public engagement. ‘6th Cluster Workshop’, ESTEC, 29 September – 3 October 2003 About 100 participants attended this workshop, consisting of three parallel splinter sessions on various topics, including collisionless shocks, magnetopause, cusps, inner magnetosphere and identification of plasma wave modes. Owing to the supersonic nature of the solar wind, a shock layer is formed in front of the Earth’s magnetosphere. The understanding of the shock essentially requires multisatellite observations. At the shock, strong electric currents flow; a typical current here is of the order of 106 A (note that this can be measured only with Cluster). 13th SOHO Workshop, ‘Waves, Oscillations and SmallScale Transient Events in the Solar Atmosphere: A Joint View from SOHO and TRACE’, Palma de Mallorca, Spain, 29 September – 3 October 2003 The 13th SOHO Workshop was held jointly with the TRACE team on waves, oscillations and small-scale transient events in the solar atmosphere. Detailed observational studies with SOHO and TRACE have provided a strong stimulus to theoretical developments, so much so that coronal seismology (the determination of coronal parameters by using information from the waves the medium supports) is rapidly developing and providing insight into some of the physical parameters and processes at work in the corona. Nearly 100 participants discussed 110 papers in seven sessions covering MHD Waves and Oscillations in Photospheric Structures, Waves in the Chromosphere, Topological Changes and Magnetic Coupling, Waves and Oscillations in Prominences, Transition Region Dynamics: Transients, Jets, Wave Acceleration in Open Magnetic Regions and Coronal Seismology. The proceedings were published by ESA SP-547. symposia and workshops ‘ILEWG5, International Lunar Conference 2003’, Hawaii, USA, 16-22 November 2003 The International Lunar Conference ILC2003 was organised under the auspices of the International Lunar Exploration Working Group (ILEWG). This meeting attracted lunar explorers at large, including Apollo astronauts John Young and Harrison Schmitt, space professionals and enthusiasts from all over the world. Among the topics discussed were the exploration and utilisation of the Moon, and issues such as exploration, science, advanced technologies, lunar resources, robotic and human expansion, lunar bases, commercialisation, Moon/Mars synergies, lunar tourism and who owns the Moon were addressed ( http://www.spaceagepub.com/ program.html). This conference was an opportunity to hear the latest news from SMART-1, the first European mission to the Moon. 37th ESLAB Symposium, ‘Tools and Technologies for Future Planetary Exploration’, ESTEC, 2-24 December 2003 With various European space missions either on their way to, or already in orbit around, exciting planetary objects, it was felt timely to reflect on experiences gained, and at the same time to set new focal points for future activities. The currently active or planned planetary missions reflect drastically different environments, ranging from a cold and dark world on a comet through quite benign conditions in orbit at Mars to hot environments around Venus and Mercury. Future expeditions may lead us to exotic worlds such as the Jovian icy moons or in situ analysis of Martian soils. There are high demands on innovative methods and on the technology needed to decipher the manifold scientific questions. The meeting was well supported by the scientific community and, as a result, a very balanced and interesting programme could be accomplished. As a warm up in the first session, an overview was presented of ESA studies on reference exploration scenarios, which are used to identify the technological needs of future planetary space missions. The challenges of spacecraft and scientific payload developments were addressed equally. Starting from this inspiring exercise, the symposium went on with innovative ideas and technological highlights in remote sensing instruments. Considerable interest was shown for in situ measurement techniques for planetary surfaces. New payload instrumentation was introduced as well as carrier systems enabling exploration strategies on a large scale. The detection of water (a prerequisite for the existence of life) and the recognition of traces of life itself are of substantial interest and were reflected in a full session. The presented concepts and technologies demonstrated the advanced level of expertise within Europe. sec3.qxd 7/15/05 10:01 AM Page 97 symposia and workshops The symposium was concluded with the Director of Science’s outlook on the future of the scientific programme. Overall, the 37th ESLAB Symposium was a great success, combining the efforts of the European science community and ESA towards the future exploration of our Solar System and beyond. ‘Moon-Mars Workshop’, Bremen, Germany, 26 28 September 2003; Vancouver, Canada, 1-8 October 2004 The Moon-Mars Workshop (MMW) was a recommendation from the Space Generation Summit (SGS) held at the World Space Congress in Houston in 2002. The Space Exploration workgroups from SGS decided that it is very important to look at current Moon and Mars exploration plans and to highlight their commonalities in order to show how developments for one benefit the other. A single roadmap is needed for Moon-Mars exploration, and this should accelerate our pace in exploration and colonisation of our near Solar System. The First MoonMars Workshop was held in Bremen in conjunction and collocated with the Third European Mars Society Conference (EMC3), in connection with the IAF. The Second Moon-Mars Workshop was held in Vancouver during IAF 2004 (http://moonmarsworkshop. com/ and http://moonmars.org/) ‘3rd VILSPA SAS Workshop’, VILSPA, Spain, 8-10 October 2003, and ‘4th VILSPA SAS Workshop’, VILSPA, Spain, 8-11 June 2004 The VILSPA Science Analysis System (SAS) Workshops provide XMM-Newton users who have little or no experience of XMM-Newton data analysis with an introduction to the procedures and techniques for reducing and analysing XMM-Newton data. No specific knowledge of X-ray data analysis is in principle required to attend the workshop. The 3-4 day workshops are organised as half-days of presentations, and half-days of practical training (hands-on) sessions. In the practical sessions, the participants, supported by XMM-Newton SOC scientists, can accomplish reduction tasks on XMM-Newton public databases, belonging to the SAS Scientific Validation or extracted from the public archive. Attendance is strictly limited to 20 people, to ensure proper individual support. 2nd Planck Symposium, ‘Setting the Scene’, Orsay, France, 28-30 January 2004 The objective of these meetings is to update the many individuals involved in all facets of Planck’s development, and to stimulate discussion across Planck-related topics. This Symposium carried the title ‘Setting the Scene’ because it was timely to take a detailed look at 97 what will be the state-of-the-art of the field at the time of Planck’s launch. The bulk of the Symposium was devoted to scientific talks on the probable scientific return of Planck in view of currently ongoing and planned experiments. These talks covered the spectrum of Planck science, not only CMB-based cosmology, but also extragalactic science, as well as the study of the Milky Way. Critical issues of instrument technology and data processing were also addressed. Finally, a large number of high-quality posters gave insight into many detailed aspects of Planck. The discussions held in the various sessions confirmed that the scientific potential of Planck remains of the highest calibre, even in view of the recent release of WMAP data, and of new and very powerful ground- or balloon-based experiments that are planned in the coming decade. Although it was clear that, in just 3 days, it was impossible to cover all the potential scientific return of Planck, the Symposium fulfilled its objectives and served as a valuable milestone on the road towards the satellite’s launch. ‘5th Integral Workshop’, Munich, Germany, 16-20 February 2004 230 participants from all over the world attended the 5th Integral workshop. Many key results from Integral observations were presented, including one very exciting result from Integral’s Galactic Plane Scan (GPS) programme: the discovery of a new type of highly obscured X-ray binary sources that had so far escaped detection with other instruments. These new sources are located within the Norma spiral arm of our galaxy. Integral also observed the centre of the Galaxy, which contains a super-massive black hole and yet only shows relatively faint emission. The discovery of a source, IGR J17456-2901, coincident with the Galactic nucleus Sgr A* to within 0.9 arcmin was reported. It is the first observation of significant hard X-ray emission from within the inner 10 arcmin of the Galaxy and a contribution from the galactic super-massive black hole itself cannot be excluded. Detection of 91 gamma-ray sources towards the direction of the Galactic centre was reported, of which 26 are new discoveries (Nature 2004, 428, 293). The sources detected by Integral account for the vast majority of the Milky Way’s (‘diffuse’) emission at soft gamma-rays observed for 30 years, leaving only a minor role for diffuse processes. After 1 year in orbit, a comprehensive survey of Integral/ IBIS Core Program survey data was presented incorporating both the GPS and GCDE. A total of 124 sources has been detected, of which 40% are low-mass X-ray binaries and 31% are of undefined nature; 14 sources are completely new. sec3.qxd 7/15/05 10:01 AM Page 98 98 The last session was devoted to Gamma-Ray Bursts (GRBs); 10 have been seen in the field of view so far. It was shown that the Integral Burst Alert System currently gives the best GRB localisations, in terms of speed and accuracy, for follow-up observation of their afterglows. ‘2nd Cluster Tail Workshop’, Mullard Space Science Laboratory, Dorking, UK, 3-5 March 2004 Some 40 Cluster scientists gathered to discuss in particular the dynamical processes of the Earth’s magnetotail. A main topic was magnetic reconnection that occurs everywhere in the Universe, but our geospace is the only place where we can monitor and investigate it in detail. Many other issues were also discussed, such as the characteristics of thin current sheets that precede the reconnection; characteristics and existence of ion beams; plasma flow reversals, flux robes, plasmoids and vorticity in the magnetotail; effects of interplanetary shocks on the magnetotail, and so on. More information about the workshop can be found at http://www.mssl.ucl. ac.uk/www_plasma/missions/cluster/7thworkshop/ ‘Titan from Discovery to Encounter’, ESTEC, 13-17 April 2004 This international conference was held on the 375th birthday of Christiaan Huygens (born 14 April 1629). During the 17th century, Huygens was one of the most respected European scientists; a highlight of his career was the discovery of Saturn’s largest moon, Titan. The aim of the conference was to bring together historians and space scientists to discuss not only Huygens the person, the scientist and his relationship with other scientists of his time, but also observations of Saturn and its moons since the 17th century, as well as coming up to date with the Cassini-Huygens mission and the latest observations on the way to encounter. The conference was attended by about 120 space scientists and historians, and the last day was open to the public, attracting more than 100 people. The proceedings were published as ESA SP-1278. ‘13th Cool Star Workshop’, Hamburg, Germany, 5-9 July 2004 The ‘Cambridge Workshop on Cool Stars, Stellar Systems and the Sun’ is the major event of the cool stars community. Organised every 2 years, it now traditionally alternates between the USA and Europe. The 13th workshop was coorganised by the University of Hamburg and RSSD. The workshop was a big success, with 293 registered participants from all over the world, making it one of the best attended since the start of the series in 1980. Among the major topics discussed were symposia and workshops the new insights into coronal physics obtained from highresolution XMM and Chandra spectroscopy, new results on stellar and planetary formation, and the impact of IR survey and spectroscopy on our understanding of lowmass stars, brown dwarfs and planets. Cool Stars 13 experimented with the format of the meeting, with the organisation of splinter sessions left to individual participants. This was a success, as all splinters were well attended. The generous sponsorship by ESA allowed the participation of a number of students and young researchers. The proceedings will be published as ESA SP-560. 38th ESLAB Symposium, ‘5th International LISA Symposium’, ESTEC, 12-16 July 2004 The 5th International LISA Symposium was held jointly with the 38th ESLAB Symposium. The Symposium traditionally focuses on the science and technology of LISA and is held every second year. The Symposium was attended by about 180 participants who discussed about 90 papers covering all aspects of LISA, starting from the state of the mission in ESA and NASA, leading through the technological aspects of LISA and its technology demonstrator LISA Pathfinder, finally coming to the astrophysics of the sources. The proceedings will be published in a special issue of Classical and Quantum Gravity. 14th SOHO Workshop, ‘Helio- and Asteroseismology: Towards a Golden Future’, Yale University, New Haven, CT, USA, 12-16 July 2004 The 14th SOHO Workshop was held jointly with the annual meeting of the Global Oscillation Network Group. It focused on the study of the interior of the Sun from a seismic perspective and the prospects for similar study of Sun-like stars. Nearly 120 participants discussed over 125 papers addressing a wide variety of topics, including the observational status of low-, medium- and high-degree p-mode characterisation, low-frequency gmode detection, solar structure and dynamics, mode excitation and damping, advances in local helioseismology, and the first results from the Canada’s MOST asteroseismology mission. The proceedings were published as ESA SP-559. ‘The Moon: Science, Technology, Utilization and Human Exploration’, COSPAR 2004, Paris, France, 22-23 July 2004 This event included solicited and contributed presentations, organised in topical sub-sessions such as sec3.qxd 7/15/05 10:01 AM Page 99 symposia and workshops 99 Science of the Moon, A Keystone for Planetary Research; Formation and Early Evolution of the Moon, Earth and Terrestrial Planets; The Moon as a Laboratory for Comparative Planetology; Current Lunar Missions: SMART-1, Lunar-A, Selene, Chandrayaan-1, South Pole Aitken Sample Return, Lunar Reconnaissance Orbiter; Astronomy from the Moon; Life Sciences on the Moon; Future Exploration and Resources Utilisation; and Astrobiology, Living and Working on the Moon and Mars. giant planets, UV/X-ray output of stars, and chemistry of nebular material. ‘Dust Disks and the Formation, Evolution and Detection of Habitable Planets’, San Diego, USA, 26-29 July 2004 (Towards Other Earths (Darwin/TPF), Heidelberg, Germany, 22-25 April 2003) 15th SOHO Workshop, ‘Coronal Heating’, University of St. Andrews, Scotland, UK, 6-9 September 2004 The second joint Terrestrial Planet Finder/Darwin conference was held in Mission Bay, San Diego, California in July 2004. Attracting about 250 participants from all over the world, it followed the very successful Heidelberg meeting in April 2003. The main purpose of this conference series is to provide a forum in which to develop the field of extrasolar planet research with respect to the two missions Darwin and TPF. NASA and ESA have recognised two primary, near-term goals in arranging these joint conferences: (1) involve the community in establishing high-level goals for TPF and Darwin; and (2) address key areas of research relevant to these ambitious missions that are important to the design and architecture of TPF and Darwin, respectively. There were three major topics for this conference. The first addressed recent results on exo-zodiacal (EZ) discs from Spitzer and other space and ground observations. Also predictions of expected and exciting new results from Spitzer, HST/ACS, Keck/LBTI Interferometers, Herschel and ground-based sub-mm telescopes on the evolution, structure, composition and frequency of debris discs in the near and more distant future were discussed. Among the issues debated were how to extrapolate from the outer zodiacal clouds (Kuiper belt) detectable with Spitzer to the inner zodiacal clouds that will be measurable with TPF or Darwin. What do the Spitzer measurements of the outer zodiacal cloud tell us about the presence or absence of planets? Secondly, the link between the physical conditions in the early solar nebula and astrobiology, e.g. how might astronomical conditions in the Hadean/Archaen periods affect the formation and evolution of life? New data from, for example, GENIE and the Keck-nuller may provide new information on the properties of zodiacal discs in the first 500 million years of a planetary system’s existence. What does a high level of exo-zodiacal emission imply in terms of bombardment and infall? What other astronomical properties of a star and planetary system might be relevant to the formation of stable, habitable planets, for example, the dynamics of Finally, an updated discussion of TPF and Darwin designs and plans was also provided by ESA and NASA. This included science requirements and technology advances as well as more generic choices recently made, such as mid-IR interferometry being the current driver in Europe, while visual coronography is the first choice of NASA. More than 130 participants presented and discussed over 140 papers addressing a wide variety of topics, organised around eight sessions covering: what is the coronal heating problem?, driving coronal heating, wave heating of the corona, kinetic aspects of coronal heating, the role of reconnection in the corona, the solar-stellar connection, plasma strands and the determination of the local heating function, and where next in the search for a solution to the coronal heating problem? The proceedings were published as ESA SP-575. ‘8th Cluster Workshop’, New Hampshire, USA, 29 September – 1 October 2004 One hundred and thirty Cluster scientists gathered to discuss the most recent scientific achievements of the Cluster mission and to chart out the next phase of the mission. During the 3-day workshop, the scientists discussed several hot-button topics in four working groups: — bow shock processes, structure, and dynamics; — physics of the inner magnetosphere; — reconnection processes at the magnetopause and in the tail; — cusp dynamics and structure and auroral processes. More information about the workshop can be found at http://atlas.sr.unh.edu/cluster8/ ‘The Three-Dimensional Universe’, Paris, France, 4-7 October 2004 This major symposium, dedicated to the scientific aspects of the Gaia mission, was held at the Observatoire de Paris, Meudon, as ‘Les Rencontres de l’Observatoire 2004’. Attended by 240 delegates, the 4-day meeting was an opportunity to present the status of the Gaia mission to the scientific community, and to hear the results of investigations carried out in the various areas of the mission over the previous 4 years. sec3.qxd 7/15/05 10:01 AM Page 100 100 Activities and overall progress of the 14 scientific working groups (from relativistic aspects of the data analysis to the quasar reference frame) formed a major part of the symposium. Various reports on the massive data analysis preparations gave a detailed perspective on the complexities and challenges facing the on-ground data treatment: the overall simulation chain, the current prototype data analysis system, Grid-related studies, and the photometric data analysis. Five participants accepted the delicate challenge of summarising the poster presentations in the various categories. This effort contributed significantly to the coverage of a large variety of topics in a limited time, and was greatly appreciated by the participants. A highlight of the Symposium was the award by the Paris Observatory of the degree of Doctor Honoris Causa to the Honorary Chair of the Scientific Organising Committee, Adriaan Blaauw, who celebrated his 90th birthday earlier in the year. Generous financial support by various organisations connected to Gaia permitted the attendance at the symposium of an unusually large representation of younger scientists (PhDs and post-docs), many of whom are already playing a key role in the preparation of the ambitious Gaia mission. Attendees also included collaborators from Greece (a new Member State of ESA) and some non-member countries (Slovenia, Lithuania, Estonia, Australia). The proceedings were published as ESA SP-576. ‘The Dusty and Molecular Universe – A Prelude to Herschel and ALMA’, Paris, France 27-29 October 2004 symposia and workshops in the optical (Hubble and large 8-10 m ground optical instruments such as ESO’s VLT), in X-rays (Chandra, XMM-Newton) and other wavebands and facilities. The meeting was organised such that the various groups working on this scientific preparation could meet and exchange their ideas, orientate their work towards the best strategies, and plan complementary goals for early science with Herschel and ALMA. About 200 participants delivered a large number of oral and poster presentations. The proceedings were published as ESA SP-577. ‘6th International Conference on Exploration and Utilisation of the Moon’, Udaipur, India, 22-26 November 2004 The 6th International Lunar Conference was hosted by PRL and ISRO, and cosponsored by ILEWG and ESA. The President of India, Dr. Abdul Kalam, addressed the meeting and made some highly relevant recommendations for international activities in exploration of the Moon, ‘for the benefit of human kind’. Discussions and presentations by 200 scientists from 17 countries focused on new and planned missions to the Moon as well as roadmap concepts for long-term exploration of the Moon and the utilisation of lunar resources. The programme included key elements of science overview and opportunities for young scientists. The programme can be found on http://www.prl.ernet.in/~ILC6/ and the conference declaration on Sci.esa.int/ilewg ‘Herschel Space Observatory Calibration Workshop: Models and Observations of Astronomical Calibration Sources’, Leiden, The Netherlands, 1-3 December 2004 The future sub-mm and far-IR facilities of Herschel and ALMA will make a breakthrough in our knowledge of star formation, the bulk of it occurring in dusty and obscured regions, that can be revealed only at these wavelengths. They will shed light on the physical processes of galaxy formation, the formation of the first stars after the dark age, starbursts in interacting and merging galaxies, and the fuelling of black holes. The physics and chemistry of the interstellar medium will be known in unprecedented detail. The production of dust and various elements in stars, supernovae and stellar winds will be tackled by the observation of the circumstellar medium. Knowledge of cometary and planetary atmospheres will be considerably enhanced, and their molecular abundances revealed. The main purpose of the workshop was to provide an overview of the state-of-the-art of models, observations and laboratory spectroscopic studies associated with Herschel calibration sources, and to facilitate the discussion between experts. The workshop brought together calibration scientists from the three Herschel instruments, members of the Herschel Science Centre and the NASA Herschel Science Centre, planetary and stellar modellers and observers, and calibration scientists from ground and space observatories that cover similar wavelength regions, in particular from ALMA, Astro-F, ISO, JCMT, Planck, SOFIA, Spitzer Space Telescope and SWAS. The scientific preparation for the utilisation of these facilities, expected to become operational just a few years from now, is already underway using the legacy of IRAS and ISO and through the presently operating ground-based (sub)mm telescopes and the recent Spitzer IR space telescope. Complementary surveys are obtained Over 45 scientists from Europe, USA and Japan attended the meeting. The workshop programme was organised in both plenary and splinter sessions. The four splinter sessions focused on the topics of Mars and giant planets, Asteroids and satellites, Stars and secondary calibrators, and Calibration and cross-calibration strategies. sec3.qxd 7/15/05 10:01 AM Page 101 symposia and workshops The talks in the plenary sessions covered subjects common across the splinters. They included presentations on the Herschel mission and of the Herschel instruments’ calibration strategies. Other talks provided overviews on the use of Solar System objects as calibrators, of the current knowledge of solid-state features in the far-IR and of the work in progress to study and model the far-IR background. The workshop achieved its objectives and definitely helped in determining the future path for the calibration preparatory work. The viewgraphs of the presentations and a list of actions identified during the meeting are collected on the workshop web page (http://www.rssd.esa.int/Herschel/ hcal_wkshop.shtml). The models and observations of astronomical calibration sources will be consolidated, documented and made available to the calibration scientists through a common database. 101 4.2 ESA Technology Programmes The ESA science directorate relies heavily on three programmes to ensure technology developments are in place to support future missions. These are: — the Core Technology Programme, funded directly from the Science Programme and covering the needs of embryonic future missions and of more mature missions either in assessment or under definition. This programme focuses on high-priority core technologies needed specifically within science and covers the complete range of technology readiness levels (TRLs 1-10). — the Technology Research Programme (TRP), funded by the ESA General Budget and accessed by all customer directorates. In general, it covers technology in the early stages of development (essentially TRL levels 1-3). — the General Support Technology Programme (GSTP), funded directly by those Member States RHESSI/SOHO/TRACE Workshop, ‘Coordinated Observations of Flares and CMEs’, Sonoma, California, USA, 8-11 December 2004 The RHESSI/SOHO/TRACE workshop was oriented towards the synthesis of data from these three missions and ground-based data. The workshop was attended by over 140 participants. With the emphasis being on actual research work, there were no set presentations other than four introductory talks. To maximise the exchange of ideas and foster new research arrangements, the workshop was organised around seven parallel working groups covering: pre-event physics; magnetic reconnection & formation of current sheets; interrelationships of flares/CMEs in ‘super’ events; solar origins of solar energetic particles; ribbons and footpoints; imaging spectroscopy of the thermal plasma; particle acceleration and transport. Figure 4.2/1: The various programmes and their relationship with the Technology Readiness Levels used within ESA. Figure 4.2/2: The overall flow of the technology planning and implementation process. TDA: Technology Development Activity. TRM: Technology Reference Mission. sec3.qxd 7/15/05 10:01 AM Page 102 102 coordination/support activities interested in a specific technology item. Generally, it matures technology for direct application and therefore covers TRL levels 4-10. Figure 4.2/1 illustrates the overall approach to these various programmes and the associated TRL level. Of course, the individual items entering the various programmes, whatever the funding approach, are crucial to the overall success. Fig. 4.2/2 illustrates this complex process, which attempts to ensure that the correct technology needs of the Science Programme are identified and eventually enter the programme at the right time. SCI-A conduct studies into test-case missions, known as Technology Reference Missions (TRMs), that examine technical feasibility, costs and technology needs. These TRMs assist the programme in providing inputs to the science community with regard to possible future projects as well as identifying core technologies, often at a very low TRL, that may need to be developed in the longer term. 4.3 Coordination and Other Supporting Activities EIROforum The EIROforum is a partnership between seven leading European intergovernmental research organisations: CERN, EFDA, EMBL, ESA, ESO, ESRF and ILL. As world leaders within their respective fields of science, the member organisations represent the vanguard of European science, proving that European scientists can be competitive at the forefront of research. These organisations have a vital role to play in the future of European research. A primary goal of EIROforum is to play an active role in promoting the quality and impact of European research through effective high-level interorganisational interaction and coordination. This is possible by exploiting the existing intimate links between the member organisations and their respective European research communities. The Head of RSSD is a member of the ESA EIROforum delegation. During the reporting period, ESA has occupied the chairmanship of the group for the last 6 months, with the Director of Science representing the Director General of ESA. In this period, a decisive push has been given to the previously existing working groups on instrumentations, grid technologies, human resources and, in particular, the preparation of a knowledge database on the management of large infrastructures. From the policy point of view, an EIROforum vision paper was prepared during the last year that is now being presented to the organisations of the European Union and, in particular, to the Science and Research Commission. AVO/EURO-VO Work continues on the development of Virtual Observatory (VO) tools in cooperation with other European organisations. After the success of the Astrovirtel programme, members of the Department in ST-ECF and ESAC are preparing the next steps in this much-needed resource for modern astrophysical research using a variety of observational databases, both groundand space-based. The last demonstration of the Astrophysical VO (AVO) project, before the beginning of the implementation of its fully-fledged form, was performed at ESAC. The use of archival data (including ISO and XMM) for this type of research was found to be particularly useful. Cooperation with ESO, through ST-ECF, as well as other astronomical centres in Europe, is envisaged in the preparation of a proposal to the European Commission for funding of some of the components of AVO. More information is given in the Divisional sections of this report. sec3.qxd 7/15/05 10:01 AM Page 103 coordination/support activities Opticon The ST-ECF, on behalf of RSSD, participated in the Opticon network. This is an ‘Integrated Infrastructure Initiative (I3)’ European Commission-funded programme that comprises networking, a trans-national access programme and a series of six technology projects called Joint Research Activities. RSSD contributes to these activities through the ST-ECF group in Garching (D); the involvement of other members of the Department is being encouraged in specific JRAs linked more closely to space projects. 103 Fellows, funded to work 1 or 2 years in ESA Member States’ institutions outside their home countries. These Fellows contribute to research networking in support of ESA missions. Research Fellows working with the ESA SOHO team at NASA/GSFC or at the STScI are also recruited via this scheme. General Scientific Support RSSD staff provided scientific advice and support to and participated in committee and working groups not directly within the purview of the Scientific Directorate or of ESA. These included: Europlanet This is a new European Commission-funded network of coordinated activities in planetary sciences. It was set up to achieve a long-term integration of this discipline in Europe. Its aims are to increase the science return of planetary projects, with emphasis on major exploration missions, to initiate a long-term improvement of the European planetary work infrastructure, to improve European scientific competitiveness, to develop and spread expertise in this area of research, and to develop public understanding of and support for planetary science and exploration. These goals will be achieved by maximising synergies between different fields contributing to planetary sciences: space observations, Earth-based observatories, laboratory studies, numerical simulations and the development of databases. In addition, the design and development of an Integrated and Distributed Information Service providing access to the full set of data sources produced by the mentioned complementary fields is a driver of the project. Astronet Very recently, members of RSSD have been involved in the preparation of a proposal to the European Commission for funding of a network of European research agencies in astronomy. Though only associated members rather than full partners, owing to the nature of ESA as a European organisation, an ambitious work plan has been designed aimed at structuring and coordinating European astronomical research. This plan is based on a number of work packages, including networking, a strategic review of European astronomy, an infrastructure roadmap and coordinated actions to strengthen astronomy and astrophysics in Europe External Research Fellows In addition to the internal Research Fellowship Programme, there are about 20 External Research — A. Gimenez is a member of the Council of the European Astronomical Society and President of the IAU Commision on Binary Stars. — G. Schwehm continued to provide support to the Agency’s Space Debris Working Group and as as coordinator for all planetary protection activities within the Agency. — in coordination with ESA’s International Affairs Department, RSSD staff have continued to provide support to the organisation and programme development of the UN/ESA Workshops on Basic Space Science. This series of workshops has found a special niche in identifying opportunities to promote space science in the developing nations, both in order to provide opportunities for professional scientists, and as a means of enhancing the role of science in the educational systems of these nations. The results of the first ten of these Workshops were summarised in the book Developing Basic Space Science World-Wide (W. Wamsteker, R. Albrecht, H. Haubold, Eds. Kluwer, Dortrecht, 2004). The 11th UN/ESA Workshop, originally scheduled for November 2003 in Beijing, China, was rescheduled owing to the SARS epidemic, and held in May 2004, hosted by the government of P.R. China and the Chinese Space Agency. The emphasis was on promoting international and regional collaboration, and access to data from high-end facilities via the Virtual Observatory. The concept of a World Space Observatory, as an effective means of stimulating space science in developing countries, and generating better opportunities for participation of scientists from developing countries in space science and education, was further pursued. Responsibility for liaison with the United Nations was transferred to R. Albrecht (ST-ECF) after the retirement of W. Wamsteker. — B.H. Foing is the ESA representative and Executive Director of the International Lunar Exploration Working Group (ILEWG), a body charged with developing and coordinating an international strategy for the exploration of the Moon. He also participated in a Cosmic Study of the International Academy of Astronautics on ‘Next Steps in sec3.qxd 7/15/05 10:01 AM Page 104 104 Exploring Deep Space’, led by Dr. W. Huntress (Carnegie), released in July 2004. The IAA study outlines compelling scientific and cultural imperatives that provide the context for a vigorous programme of robotic science missions and for a systematic and evolutionary architecture for human expansion into the Solar System. — RSSD staff were active in numerous scientific societies (EAS, EGS, EPS) and some of the Scientific Unions (COSPAR, IAU, IRSI, IUPAP), where they contributed to scientific meetings by organising special sessions and discussions, and, in some cases, holding elective offices. For example, H. Svedhem is a member of EGU Council and President of the Geophysical Instrumentation Section of the EGU. — RSSD staff also taught space sciences and related topics in Member State universities and in several instances were also appointed as jury members for Ph.D. theses. The direct contact between ESA staff and students and staff at the Universities continues to be mutually rewarding. science communications 4.4 Science Communications Supporting the ESA Corporate and Science Communication Services RSSD Project Scientists and staff supported a number of science communication activities related to their projects. These include text and pictures for leaflets, posters and brochures, and contributions to 80 web stories in 2003 and 67 stories in 2004 for the ESA public website (www.esa.int) and ESA space science pages (www.esa.int/esaSC). Of the more than 90 and 140 ESA press releases in 2003 and 2004, respectively, 79 and 67 were related to science. In addition, more than 82 press releases were issued by STScI over the 2 years. A large effort was made by RSSD staff to support the development, input updating and maintenance of the ESA scitech website (sci.esa.int), aimed at the scientific and educated communities, with specific information on all missions: status reports, announcements, upcoming events, latest publications, mission background, science, spacecraft and science operations, services, image gallery and videos. The Chief Scientist proposed an overall structure for the thematic contents of the scitech site. RSSD staff (in particular, Project Scientists) supported ESA Corporate PR services in the production of TV broadcast material related to ESA science missions, in a variety of formats: documentaries for the general public; documentaries for the technical public; Index, A- and Brolls; video Index, chapter structured; Interviews; Video News Releases; and live action. This material was distributed by ESA PR at related events or broadcast on ESA TV to European channels. Contents of ESA Science Communication Stories for the Public in 2003-2004 ESA’s PR emphasis is often directed towards launch campaigns. RSSD Project Scientists supported ESA PR offices, in coordination with project teams, by preparing material, text and pictures for stories about these science missions from complementary viewpoints at selected milestones: the science background and goals, preparation and key events for the spacecraft, specific instruments and technologies, initial results and more complete results. Mars Express was the subject of 51 web stories in 20032004, including the preparation for launch in June 2003, the arrival at Mars on 25 December, the search for Beagle-2 and the related enquiry, and the results from the orbiter. These included the spectacular stereo imagery of Mars’ geology, volcanoes, water features, impact craters, the detection of polar water ice by the instruments, the detection of methane by the Planetary Fourier Spectro- sec3.qxd 7/15/05 10:01 AM Page 105 science communications meter, water loss in the atmosphere, evidence for recent volcanism and glacial activity. RSSD staff supported a number of press events, covering both mission aspects and research. The communications activities on SMART-1 included promotion of lunar and planetary science, new technologies, people and new methods for small space missions, and exploration. The Project Scientist supported film crews working on interviews and documentaries on SMART-1 and lunar exploration. He supported media briefing events in March 2003, as well as the pre-launch campaign in September 2003. The first results from the commissioning, cruise, navigation and lunar capture on 15 November 2004 were featured. The SMART-1 team collaborated with ILEWG (sci.esa.int/ ilewg) and the Lunar Explorers Society, (lunarexplorer. org) in public events. PR events were organised at the ILEWG conferences in Hawaii (2003) and Udaipur, India (2004) in the presence of Apollo astronauts and the President of India, respectively. The Cassini/Huygens arrival at Saturn prompted 10 stories on the critical Saturn orbit insertion, four from Cassini flybys (Phoebe, Titan, new moons) and the preparation for the release of Huygens over Christmas 2004, building up the interest for the 14 January 2005 atmospheric entry and landing. Rosetta also enjoyed high PR activities during 20032004, with 19 web stories emphasising the launch campaign, the delay to 2004 and the environmental testing, as well as the science involved, such as the origins of the Solar System and the delivery from comets of the ingredients for life. RSSD staff also contributed to educational and outreach activities related to astronomical events such as lunar eclipses, the Mercury transit in May 2003 and the Venus transit on 8 June 2004. Observations and discoveries made with SOHO have continued to make the headlines, with a number of CNN news stories. Special stories include the giant Halloween superflare of October-November 2003, and the detection (mostly by amateurs) of more than 750 comets with SOHO. The solution of the high-gain antenna problem was also newsworthy. Articles about SOHO have appeared in several popular magazines. Several film and TV crews visited the operations facility, and SOHO was featured in a number of science TV programmes. SOHO observations and images play a prominent role in the 40min giant-screen IMAX documentary ‘SOLARMAX’ (www.solarmovie.com). Astronomy missions had a modest level of PR and ESA science communication activities, with seven ESA press releases and 10 web stories in 2003-2004. Themes included X-ray astronomy, with stories on stellar coronae 105 and cycles, clusters of galaxies, dark energy, accretion onto rotating black holes and dead-star magnetism. With Integral, the stories included the hot trail of Geminga, gamma-ray bursts, hidden black holes, and the new view of the Milky Way. The ESA website also mirrored or expanded some of the HST stories and imagery from STScI. In addition, some HST stories from STScI exploited the use of spectacular images, such as the light echo around an erupting star. Some general astronomical stories were produced on virtual observatories, the space grid, the search for exoplanets, star formation, origin of the Universe, mapping the Milky Way and preparing the background for the upcoming Herschel, Planck, Gaia and JWST observatories. RSSD scientists supported a large number of other communication activities during 2003-2004, including: — Le Bourget, Farnborough and other space fairs. Animations included presentations on space science and technology for the press and the public, 3-D visualisations and demonstration models from some ESA space missions. — RSSD Project Scientist staff organised or supported science communication events aimed at the science community at large during sessions at the EGU in Nice, IAF in Bremen and Vancouver, COSPAR in Paris, IAU, the JENAM joint European astronomy meeting, and national astronomy meetings. They assisted in the organisation of a number of exhibition events (co-sponsored by ESA) featuring ESA space science missions. — RSSD staff contributed ESA space science communication activities (highlights from ESA science missions, lunar and planetary exploration, astronomy, space science, etc.) at press conferences, and scientific and public assemblies (COSPAR, EGS/EGU, IAF, IAU). — RSSD staff supported collaborative science communication events with museums, planetariums and educational institutions all over Europe. A network of space science communication partners was further developed, such as the British Festival of Science, Space Week and the Association of Science Journalists. Supporting Education, Teachers and Student Outreach Initiatives RSSD participated in outreach activities such as the ‘Physics on Stage’ events for teachers at ESTEC in November 2003, and Life in the Universe, Moon, Mars, planetary and astronomy workshops. They provided lectures and tutoring as part of the ESA student initiative that allowed the participation of 300 students at IAF Bremen in October 2003 and IAF Vancouver in October sec3.qxd 7/15/05 10:01 AM Page 106 106 2004. They also served as lecturers and as reviewers in student projects coordinated by the ESA Outreach and Education Office. They advised the Education Office on the science background of hands-on projects for students. Public outreach activities were conducted during astronomical events such as the Mercury and Venus transits. They contributed lectures during conferences, public events, festivals of science, and university and institute general lectures and open days. ESA Science and Technology Website (Missions and News): http://sci.esa.int ESA corporate portal: www.esa.int, with public science website: www.esa.int/esaSC ILEWG site: http://sci.esa.int/ilewg/ HST news site: http://hubblesite.org science communications sec4.qxd 7/12/05 9:52 AM Page 107 ANNEX 1 Manpower Deployment sec4.qxd 7/12/05 9:52 AM Page 108 108 manpower deployment ANNEX 1: MANPOWER DEPLOYMENT Department Office, ESTEC Head of Department Gimenez, A. Chief Scientist Foing, B.H., SMART-1 Project Scientist, comparative planetary and astrobiology, solar-stellar physics. Administrative staff Bingham, C., Departmental Assistant Administrator Ihaddadene, S., Divisional Secretary and Admin. Assistant Schroeder, B., Divisional Secretary and Admin. Assistant Villien, C., Divisional Secretary and Admin. Assistant Project Controllers (seconded from SCI-M) D’Aquino, G. Davis, R. Fontaine, R. Astrophysics Missions Division Clavel, J., Head of Division, Multiwavelength observational astronomy. Boeker, T., (from September 2003), JWST Scientist, Galaxy formation and evolution De Bruin, J., Gaia Support Scientist Favata, F., Eddington Study Scientist, COROT Project Scientist, support to Gaia studies, cool stars and stellar activity, X-ray astronomy Fridlund, M., IRSI/Darwin Study Scientist, astrophysics of star formation Heras, A., Herschel scientist, IR astronomy Jakobsen, P., JWST Study Scientist, optical/UV astronomy with HST and ground-based astronomy Laureijs, R., Planck Deputy Project Scientist, interstellar medium, dust properties Leeks, S., (from April 2003), Herschel Instrument and Calibration Scientist Marston, A., (from April 2003), Herschel Instrument and Calibration Scientist Parmar, A., Acting Integral Project Scientist, XEUS, Lobster, Rosita & EUSO Study Scientist, Leader for the SAX LEGSPC, X-ray astronomy (X-ray binaries and AGNs) Perryman, M.A.C., Hipparcos Project Scientist, Gaia Project Scientist, exploitation of Hipparcos data Pilbratt, G.L., Herschel Project Scientist, IR and sub-mm astronomy Prusti, T., Herschel Scientist, IR astronomy Tauber, J., Planck Project Scientist, sub-mm astronomy Vavrek, R., (from April 2004), Herschel Instrument and Calibration Scientist ESA Research Fellows Boirin, L., (to September 2003), X-ray astronomy Del Burgo, C., (to September 2004), Modelling of sky as seen by Planck Diaz Trigo, M., (from May 2004), Data analysis concentrating on study of stellar coronae and absorption lines in compact sources Dupac, X., (to October 2004), Planck-related science on cosmic background and interstellar dust Hony, S., (to January 2005), Interstellar medium, circumstellar envelopes, dust Husain, G., (from October 2003), Stellar activity, coronae McBreen, S., (from October 2004), Analysis of Integral and XMM data on compact accreting sources Papadopolous, P., (to March 2003), Interstellar medium Sanz Forcada, J., (from February 2004), Asteroseismology Stankov, A., (to January 2004), analysis of stellar seismology Spanish/Portuguese Trainees Perez-Ramirez, D., (to January 2004), Reduction of XMM-Newton data Silva, B., (to October 2004), Computer model to simulate number and distribution of planets that Eddington could find Solar and Solar-Terrestrial Missions Division Opgenoorth, H., (from April 2003), Head of Solar and Solar-Terrestrial Missions Division Brekke, P., (to November 2004), Support to SOHO Project Scientist, solar physics, science communication Escoubet, C.P., Cluster and Double Star Project Scientist, magnetospheric physics Fehringer, M., (to March 2003), Support to Cluster and Double Star Project Scientist, Microscope Study Scientist (under the Fundamental Physics Missions Division) Fleck, B., SOHO Project Scientist, Solar Orbiter Study Scientist, solar physics Haugan, S., SOHO Science Operations Coordinator, solar physics Marsden, R.G., Ulysses Project Scientist and Project Manager, Solar Orbiter Study Scientist, ILWS support, energetic particle data interpretation Sanchez, L., SOHO Science Data Ordinator, SOHO archive Sanderson, T.R., Cluster Archive Scientist, energetic particle instrument development and data interpretation sec4.qxd 7/12/05 9:52 AM Page 109 manpower deployment ESA Research Fellows Khan, H., (from August 2004), Magnetospheric physics research based on analysis of Cluster data Pitout, F., (to December 2004), Magnetospheric research based on analysis of Cluster data Regnier, S., (from February 2004), Study of structure and dynamics of solar surface fields (EU Fellow) ESA External Fellow McIntosh, S., (to February 2003), Criticality of solar flares and chromospheric dynamics Planetary Missions Division Schwehm, G., Head of Division, Rosetta Project Scientist Chicarro, A., Mars Express Project Scientist, planetary geology Grard, R.J.L., (to November 2003), BepiColombo Project Scientist, modelling and instrument development Koschny, D., Support to Rosetta Project Scientist, science operations planning, meteor research, planetary cameras Laakso, H., (from April 2003), Support to Cluster, magnetospheric plasma research Lebreton, J.-P., Huygens Mission Manager, Solar System technology support, plasma physics instrument development Martin, P., Mars Express Operations Scientist Ocampo, A., (to February 2004), Support to Mars Express and BepiColombo Schulz, R.M., Bepi Colombo Project Scientist (from 2003), cometary studies Svedhem, L.H., Venus Express Project Scientist, development of planetary instrumentation, cosmic dust studies Witasse, O., Huygens, planetary atmospheres Wirth, K., (from August 2003), Planetary Scientist/Applied Physicist Research Fellows Boudin, N., (to February 2004), Astrochemistry Campbell, M., (to December 2003), Observations and monitoring of meteors Cord, A., (from October 2004), Analysis of imaging Mars Express data Davidsson, B., (from May 2003), Comet nuclei thermophysical modelling and observations Makinen, J., (to December 2003), Cometary science (data analysis and modelling) Michael, G., (to April 2004), Comparative planetology. Piot, A., (to February 2004), exploitation of Huygens test balloon data Zegers, T., (from May 2003), Geology and hydrology of Mars with Mars Express 109 Young Gradutate Trainees Conan, Y., (to April 2004) Merikallio, S., (from August 2004), Spacecraft charging Sarkarati, N., (from May 2004), Experiment modelling Spanish/Portuguese Trainees Almeida, M., (from April 2003), SMART-1 AMIE calibration, science operations support Perez Ayucar, M., (to June 2004), Telecommunication Engineer – Huygens Simoes, F., (to September 2004), Water on Mars Vazquez Garcia, J.L., (to May 2004), Telecommunications Engineer – SMART-1 Stagiaires Andurand, P., (March-September 2003) Civeit, T., (April-September 2003) Couturier-Doux, S., (April-October 2004) Maloreau, S., (March-August 2003) Nicoll, R., (February-April 2003) Piberne, R., (April-October 2004) Roussos, E., (April-July 2004) Sarmiento Ares, E., (March-August 2004) Seoane Purrinos, L., (March-August 2004) Van Kan, M., (March-August 2004) Vicente, D., (March-August 2003) Zeyen, B., (April-July 2003) Fundamental Physics Missions Division Reinhard, R., Head of Fundamental Physics Division, LISA Pathfinder Project Scientist Caccapuoti, L., (from December 2004), ACES Project Scientist (for D/HME) Fehringer, M., MICROSCOPE Study Scientist (to March 2003) Jafry, Y., (to August 2004), drag-free control expert for fundamental physics missions Jennrich, O., LISA Project Scientist Space Telescope Operations Division Macchetto, D., Head of Division, AGN, Elliptical galaxies, gamma-ray bursts ST-ECF, Garching ESA scientific staff Benvenuti, P., (to October 2004), HST Project Scientist, Head of ECF, extragalactic HII regions, SNRs Albrecht, R., Deputy Head ECF, Head of Science Data and Software Group, minor bodies of the Solar System, computer science Dolensky, M., (to January 2003), Science archive and WWW software specialist Fosbury, R.A.E., Head of HST User Support Group, galaxies and AGNs sec4.qxd 7/12/05 9:52 AM Page 110 110 Micol, A., Science Archive Software Specialist, image processing techniques and information systems Rosa, M.R., Head Post-operational Archive Group, HII regions, star formation, supernovae, evolution of galaxies Sforna, D., Science Programmer, Systems Analysis ESO staff (included here to give the full picture of ST-ECF team staffing) Freudling, W., Instrument Scientist, observational cosmology, peculiar motion of galaxies Haase, J., Astronomical Data Archive and Pipeline Software Specialist Hook, R.N., HST Data Analysis Scientist, scientific software support, image restoration applications Kuntschner, H., Instrument Scientist, galaxy formation and evolution Pierfederici, F., ASTROVIRTEL Support Scientist Pirenne, B., HST Archive Scientist, data storage technology, gravitational lenses Pirzkal, N., Scientific Analyst/Programmer, pre-mainsequence stars Sjöberg, B., ST-ECF Admin. Assistant / Secretary Walsh, J.R., Instrument Scientist, planetary nebulae, HII regions manpower deployment gravitational lensing and cosmology, stellar dynamics, photometry Miebach, M., Lead Engineer for Scientific Instruments Mobasher, B., STIS Instrument Scientist, Galaxy surveys, dwarf galaxies, elliptical galaxies Padovani, P., (to August 2003), Multi-Mission Archive Scientist, AGN: unified schemes, evolution, X-ray spectra, blazars Panagia, N., NGST Science Lead, stars, interstellar medium, supernovae, galaxies, cosmology Robberto, M., WFC3 Instrument Scientist, star formation, massive stars, IR instrumentation Sirianni, M., ACS Instrument Scientist Stanghellini, L., (to April 2004), Proposal Scientist, planetary nebulae and their central stars, extragalactic distance scale Villaver, E., (from February 2004), Astronomer Wiklund, T., NICMOS Instrument Scientist, AGN, Starburst Galaxies ESA External Research Fellows van Bemmel, I., (from March 2003) Science Operations and Data Systems Division ESO staff under ESA contract Alexov, A., Post-Operation Instrument Scientific Programmer Bristow, P., Post-Operation Instrument Scientific Programmer Christensen, L., HST Outreach Astronomer Fourniol, N., Archive Operator Kerber, F., Post-Operation Instrument Scientist, earlytype stars Kornmesser, M., HST Outreach Technical Editor Pasquali, A., Instrument Scientist, stellar winds, nebulae STScI, Baltimore Aloisi, A., STIS Instrument Scientist Arribas, S., NICMOS Instrument Scientist, AGN, highredshift galaxies, cosmology Boeker, T., (to August 2003), NICMOS Instrument Scientist, galaxy formation and evolution, in particular gas dynamics in the central regions Clampin-Nota, A., Deputy Head, Science Division, massive stars, late stages of stellar evolution, IMF studies De Marchi, G., (to 2003), ACS Instrument Scientist, initial mass function, globular clusters, dark matter haloes Jenkner, H., HST Mission Deputy, Guide Star Catalog II, microvariability studies using FGS photometry Kamp, I., (from May 2004), Astronomer Mais-Appellaniz, J., Spectrographs Instrument Scientist, HII regions, young clusters Meylan, G., (to August 2004), Proposal Scientist, Staff Kessler, M.F., Head of Division, Infrared Astronomy Bennett, K., Gamma-ray astronomy, Planck (Co-I) Jansen, F., XMM-Newton/Mars Express Mission Manager, X-ray astronomy Szumlas, M., Technical coordination, Data Bank maintenance Thoerner, G., Divisional system analyst/computer manager, SAX data analysis and cosmology studies Toni, A., Senior data technician Winkler, C., Integral Project Scientist, gamma-ray astronomy data analysis Wamsteker, W., (to November 2004), Multidisciplinary scientist, active galaxies, abundances at high redshifts (located at Vilspa) Zender, J.J., Data handling/archiving management for planetary science operations Research Fellows Sanz Forcada, J. (from February 2004), Data analysis on physics of stellar coronae and absorption Herschel Science Centre, ESTEC Staff Riedinger, J., Herschel Science Centre Development Manager Mathieu, J-J., Interactive Analsysis (p.t., TOS support) Ott, S., System Analyst, Interactive Analysis Coordinator Prades-Valls, R., Quality Assurance (p.t., TOS support) sec4.qxd 7/12/05 9:52 AM Page 111 manpower deployment Integral Science Operations Centre (ISOC) Staff Hansson, L., Integral Science Operations Manager Barr, P., Operations scientist, mission planning Much, R., (to August 2004), Operations scientist and Deputy Project Scientist, Observational astronomy O’Rourke, L., (from September 2004), Science Operations Engineer (ESAC) Orr, A., Operations scientist, JEM-X and OMC expert, responsible for helpdesk Sternberg, J., System engineering, ISDC liaison Integral Science Data Centre (Geneva) Staff Texier, D., (to August 2004), Resident Engineer ISO Data Centre (IDC), (ESAC) Staff Garcia-Lario, P., ISO Resident Astronomer, crosscalibration expert, Handbook co-editor, late stages of stellar evolution Gry, C., (to October 2004), ISO Resident Astronomer, LWS expert, LWS Handbook, interstellar medium Lorente, R., ISO Resident Astronomer, ISOCAM expert Peschke, S., (to April 2003), ISO Resident Astronomer, ISOPHOT expert, comets Salama, A., ISO Project Scientist SWS expert, Titan, novae and symbiotic stars Verdugo, E., Resident Astronomer, ISOPHOT expert, ISO Data Archive products quality Research Fellows Garcia-Hernandez, A., (from September 2004), analysis of stellar ISO archival data Sanchez Fernandez, C., (to April 2004), ISO and XMMNewton data analysis Young Gradutate Trainee Carter, J., (from May 2004), Astronomer Spanish Trainee Del Mar Siere Gonzalez, M., (to Novembre 2004), ISO data reduction and XMM-Newton RGS wavelength calibration XMM-Newton SOC (VILSPA) Staff Altieri, B., Software and payload support, observational astronomy Arpizou, M., Secretarial and administrative support Ehle, M., XMM-Newton user support, observational astronomy Gabriel, C., XMM-Newton instrument support, supernova remnants, cosmology Guainazzi, M., XMM-Newton user support, observational astronomy Kirsch, M. EPIC Calibration Scientist Metcalfe, L., XMM-Newton Science Support Manager Munoz Peiro, J., Instrument Operations Manager 111 Pollock, M. RGS Calibration Scientist Santos-Lleo, M., XMM-Newton user support, observational astronomy Schartel, N., XMM-Newton User Support and Mission Planning Group Team Leader, observational astronomy Research Fellows Bianchi, S., (from October 2004), XMM-Newton data analysis of AGN Gimenez Bailon, E., (from May 2003), Seyfert High Energy Piconcelli, E., (from April 2003), Study of AGN Science Archives Group (VILSPA) Staff Arviset, C., System engineering. Archive group leader Mars Express Staff Texier, D., (from August 2004), Mars Express Science Operations Coordinator Science Payload and Advanced Concepts Office Peacock, A., Head of Office, STJ Research Team Leader Andersson, S., Electronics engineering for advanced technologies for semiconductors sensors Appourchaux, T., Solar Orbiter payload support, solar research. COROT instrument Research Team Leader Adriaens, M., (to June 2002), Mechnical engineer Arends, H., Mechanical engineer and mechanical laboratory coordinator Bavdaz, M., Advanced technologies sensors and optics, Sensors and Optics Research Team Leader, Head of Advanced Technology Section (p.i.) Beaufort, T., Electronics engineer for COROT PDU Biezen, J.F. van der, Electronics and laboratory metrology support to advanced technology programme. Butler, B.A.C., Instrument development engineer Dordrecht, A. van., Advanced Sensors electronics engineer Erd, C., Sensor research and development, ESA missions support Falkner, P., Electronics research and development, Head of Planetary Exploration Section (p.i.) Gondoin, Ph., Darwin-Genie instrument manager, XMM observational research Heida, J., Instrument support engineer Jolander, B., Head of Instrument Support Group, instrument development engineer Klinge, D., Instrument development engineer Lumb, D., Advanced sensor research, XEUS and ISS payload and mission support, XMM observational research sec4.qxd 7/12/05 9:52 AM Page 112 112 Martin, D., SCAM3 instrument manager, Head of Infrastructure Section (p.i.) Rando, N., Payload support and development engineer. Head of Missions Section (p.i.) Romstedt, J., In-situ planetary instrument development, Rosetta-MIDAS (AFM) Lead Scientist Smit, L.C., Instrument development support engineer Telljohann, U., Instrument electronics engineer Verveer, J., Laboratory cryogenic systems support Research Fellows Molster, F., Rosetta-MIDAS AFM Stagiares Kilter, M., (August 2003-January 2004) Kozak, R., (July-August 2003) Larfors, K. Leyder, J.-C., (January-March 2004) Trainees Moreira, O., (Portuguese Trainee from April 2002), Helioseismology Pitcher, K., (June-August 2001), International Law RSSD acknowledges the valuable contribution made by the contractor staff to the work of the Department. Erratum from previous Report (2001-2002): Head of Astrophysics Division (to October 2001) and Acting Head of Department (to May 2001); Taylor, B.G. manpower deployment sec4.qxd 7/12/05 9:52 AM Page 113 ANNEX 2 Publications sec4.qxd 7/12/05 9:52 AM Page 114 114 ANNEX 2: PUBLICATIONS Head of Research and Scientific Support Department Refereed Journals, 2003 Claret, A., Willems, B., Gimenez, A., Unveiling the internal constitution of components of close binary systems, 2003, Recent Research and Development in Astronomy and Astrophysics, 375. Clausen, J.V., Storm, J., Larsen, S.S., Gimenez, A., Eclipsing binaries in the Magellanic Clouds. uvby CCD light curves and photometric analyses for HV 982 (LMC), HV 12578 (LMC), HV 1433 (SMC), and HV 11284 (SMC), 2003, A&A, 402, 509-530. Domingo, A., Caballero, M.D., Figueras, F., Jordi, C., Torra, J., Mas-Hesse, J.M., Giminez, A., Hudcova, V., Hudec, R., The Input Catalogue for the OMC camera onboard INTEGRAL, 2003, A&A, 411, L281-L289. Gimenez, A., Lund, N., Preface, 2003, Adv. Space Res., 31/Issue 2, 275. Mas-Hesse, J.M., Gimenez, A., Culhane, J.L., Jamar, C., McBreen, B., Torra, J., Hudec, R., Fabregat, J., Meurs, E., Swings, J.P., Alcacera, M.A., Balado, A., Beiztegui, R., Belenguer, T., Bradley, L., Caballero, M.D., Cabo, P., Defise, J.M., Diaz, E., Domingo, A., Figueras, F., Figueroa, I., Hanlon, L., Hroch, F., Hudcova, V., Garcia, T., Jordan, B., Jordi, C., Kretschmar, P., Laviada, C., March, M., Martin, E., Mazy, E., Menendez, M., Mi, J.M., de Miguel, E., Munoz, T., Nolan, K., Olmedo, R., Plesseria, J.Y. Polcar, J., Reina, M., Rnotte, E., Rochus, P., Sanchez, A., San Martin, J.C., Smith, A., Soldan J., Thomas, P., Timon, V., Walton, D., OMC – An Optical Monitoring Camera for INTEGRAL. Instrument and Description, 2003, A&A, 411, L261L268. Ribas, I., Solano, E., Masana, E., Giminez, A., Effective temperatures and radii of planet-hosting stars from IR photometry, 2003, A&A, 411, L501-L504. Head of Research and Scientific Support Department Proceedings and other Publications 2003 Favata, F., Gimenez, A., The Eddington Mission (co-authored by the Eddington Science Team), 2003, Solar and Solar-like Oscillations – Insights and Challenges for the Sun and Stars, 25 th Meeting of IAU, Joint Discussion 12, JD12E, 51F. Gimenez, A., The Future of Optical Astronomy in ESA’s Science Programme, 2003, ASP Conf. Proc. Hubble’s Science Legacy – Future Optical/Ultraviolet Astronomy from Space, 136-2, 22. Gimenez, A., Concluding Remarks and Future, 2003, Extragalactic Binaries, 25th meeting of the IAU, Joint Discussion 13, 18 July 2003. Sydney, Australia, JD13E, 31G. Gimenez, A., Eclipsing Binaries and Stellar Astronomy, publications 2003, New Directions for Close Binary Studies: The Royal Road to the Stars, 3, 19. Ribas, I., Jordi, C., Vilardell, F., Guinan, E.F., Hilditch, R.W., Fitzpatrick, E.L., Valls-Gabaud, D., Gimenez, A., Properties and Distances of Eclipsing Binaries in M31, 2003, Extragalactic Binaries, 25th meeting of the IAU, Joint Discussion 13, JD123E, 35R. Shaver, P.A., Dilella, L., Gimenez, A., Astronomy, Cosmology and Fundamental Physics, 2003, Proc. ESO-CERN-ESA Symposium, ESA. Silver, E.H., Schnopper, H.W., Jones, C., Forman, W., Bandler, S.R., Murray, S.S., Romaine, S.E., Slane, P.O., Grindlay, J.E., Madden, N.W., Beeman, J.W., Haller, E.E., Smith, D.M., Barbera, M., Collura, A., Christensen, F.E., Ramsey, B.D., Woosley, S.E., Diehl, R., Tucker, G.S., Fabregat, J., Reglero, V., Gimenez, A., B-MINE, the balloon-borne microcalorimeter nuclear line explorer, 2003, X-ray and Gamma-ray telescopes and Instruments for Astronomy, Proc. SPIE, 4851, 905-912. Head of Research and Scientific Support Department Refereed Journals, 2004 Ribas, I., Jordi, C., Vilardell, F., Gimenez, A., Guinan, E.F., A program to determine a direct and accurate distance to M31 from eclipsing binaries, 2004, New Astronomy Reviews, 48/9, 755-758. sec4.qxd 7/12/05 9:52 AM Page 115 publications Astrophysics Missions Division Refereed Journals, 2003 Bendo, G.J., Joseph, R.D., Wells, M., Gallais, P., Haas, M., Heras, A.M., Klaas, U., Laureijs, R.J., Leech, K., Lemke, D., Metcalfe, L., Rowan-Robinson, M., Schulz, B., Telesco, C., Dust Temperatures in the Infrared Space Observatory Atlas of Bright Spiral Galaxies, 2003, AJ, 125, 2361. Benjamin, R.A., Churchwell, E., Babler, B.L., Bania, T.M., Clemens, D.P., Cohen, M., Dickey, J., Indebetouw, R., Jackson, J.M., Kobulnicky, H.A., Lazarian, A., Marston, A.P., Mathis, J.S., Meade, M.R., Seager, S., Stolovy, S.R., Watson, C., Whitney, B.A., Wolff, M.J., Wolfire, M.G., GLIMPSE. I. An SIRTF Legacy Project to Map the Inner Galaxy, 2003, PASP, 115, 953. Boirin, L., Parmar, A.N., Discovery of narrow X-ray absorption features from the low-mass X-ray binary X 1254-690 with XMM-Newton, 2003, A&A, 407, 1079. Boirin, L., Parmar, A.N., Barret, D., Paltani, S., Discovery of X-ray absorption lines from the lowmass X-ray binaries 4U 1916-053 and X 1254-690 with XMM-Newton, 2003, Nuclear Physics B Proceedings Supplements, 132, 506. Bridge, C.M., Cropper, M., Ramsay, G., de Bruijne, J.H.J., Reynolds, A.P., Perryman, M.A.C., Variability of the accretion stream in the eclipsing polar EP Dra, 2003, MNRAS, 341, 863. Carpano, S., Aigrain, S., Favata, F., Detecting planetary transits in the presence of stellar variability. Optimal filtering and the use of color information, 2003, A&A, 401, 743. Corbett, E.A., Kewley, L., Appleton, P.N., Charmandaris, V., Dopita, M.A., Heisler, C.A., Norris, R.P., Zezas, A., Marston, A., COLA. II. Radio and Spectroscopic Diagnostics of Nuclear Activity in Galaxies, 2003, ApJ, 583, 670. Cropper, M., Barlow, M., Perryman, M.A.C., Horne, K., Bingham, R., Page, M., Guttridge, P., Smith, A., Peacock, A., Walker, D., Charles, P., A concept for an STJ-based echelle spectrograph, 2003, MNRAS, 344, 33. Del Burgo, C., Laureijs, R.J., Abraham, P., Kiss, C., The far-infrared signature of dust in high latitude regions, 2003, MNRAS, 346, 403. Dupac, X., Bernard, J.P., Boudet, N., Giard, M., Lamarre, J.M., Miny, C., Pajot, F., Ristorcelli, I., Serra, G., Stepnik, B., Torre, J.P., Inverse temperature dependence of the dust submillimeter spectral index, 2003, A&A, 404, L11-L15. Dupac, X., Del-Burgo, C., Bernard, J.P., Giard, M., Lamarre, J.M., Laureijs, R.J., Pajot, F., Ristorcelli, I., Serra, G., Tauber, J., Torre, J.P., The complete submillimetre spectrum of NGC 891, 2003, MNRAS, 344/1, 105. 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Astrophysics Missions Division Proceedings and other Publications, 2004 Cadolle Bel, M., Goldwurm, A., Rodriquez, J., Goldini, P., Corbel, S., Sizin, P., Parmar, A.N., Kuulkers, E., Capatanao, F., Del Sanot, M., Ubertini, P., Roques, J.P., Bouchet, L., Farinelli, R., Frontera, F., Westergaard, N.J., INTEGRAL, XMM-Newton and RossiXTE observations of the state transition of the X-ray transient and black hole candidate XTE J1720-318, 2004, The 5th INTEGRAL Workshop – The INTEGRAL Universe, ESA SP-552, 215. Cassinelli, J.P., Neiner, C., Discussion session on magnetic fields and Be stars, 2004, The nature and evolution of disks around hot stars, (Accepted for Publication). Catala, C., Aricha, A., Boulade, O., Diaz, E., Epstein, G., Favata, F., Horne, K., Kjeldsen, H., Lumb, D., MasHesse, M., Roxburgh, I., Science requirements and their translation into instrumental design, 2004, Second Eddington Workshop: Stellar structure and habitable planet finding, ESA SP-538, 39. Clavel, J., The Herchel submm Space Observatory, 2004, The interplay among Black Holes, Stars and ISM in Galactic Nuclei – Proceedings IAU Symposium #222, 2004, 553. Fridlund, C.V.M., Darwin – the scientific constraints, 2004, Second Eddington Workshop: Stellar structure and habitable planet finding, 9-11 April 2003, Palermo, Italy., ESA SP-538, 225. Hussain, G.A.J., Stellar surface imaging – mapping brightness and magnetic fields, 2004, Astronomische Nachrichten, 325, 216. Kuulkers, E., Bodaghee, A., Foschini, L., Guainazzi, M., Matt, G., Israel, G., Nicastro, F., Oosterbroek, T., Parmar, A., Rodriquez, J., Walter, R., GX 339-4 detected by INTEGRAL, 2004, Astronomical Telegram, 240, 1. Lim, T., Swinyard, B., Aramburu, A., Bock, J., Ferlet, M., Griffin, D., Griffin, M., Hargrave, P., King, K., Leeks, S., Naylor, D., Ronayette, S., Sawyer, E., Schulz, B., Sidher, S., Spencer, L., Smith, D., Woodcraft, A., First Results From Herschel-SPIRE Performance Tests, 2004, Proceedings of SPIE. Optical, Infrared, and Millimeter Space Telescopes, 5487, 460-468. Neiner, C., Hubert, A.M., Magnetic fields in Be stars, 2004, The nature and evolution of disks around hot stars, (Accepted for Publication). Oosterbroek, T., Parmar, A.N., Rens, N., Israel, G.L., Stella, L., Mereghetti, S., Haberl, F., Angelini, L., 119 Non-detection of the cyclotron line in the spectrum of the anomalous X-ray pulsar 1RXS J170849-400910, 2004, The 5th INTEGRAL Workshop – The INTEGRAL Universe, ESA SP-552, 471. Parmar, A.N., Cosmology with ESAs Future HighEnergy Astronomy Programme, 2004, Proc. Mykonos Conference on Multi-wavelength Cosmology, 301, 305. Parmar, A.N., Arnaud, M., Barcons, X., Bleeker, J., Hasinger, G., Inoue, H., Palumbo, G., Turner, M., Science with XEUS – the X-ray Evolving Universe Spectroscopy Mission, 2004, Proceedings SPIE – UV and Gamma-Ray Space Telescope Systems, 5488, 388. Peeters, E., Allamandola, L.J., Hudgins, D.M., Hony, S., Tielens, A.G.G.M., The Unidentified InfraRed Bands after ISO, 2004, Astrophysics of Dust, Estes Park, Colorado, May 26-30, 2003, 309, 141. Perryman, M.A.C., Detection and Characterization of Extra-Solar Planets, 2004, The Search for Other Worlds, 713, 283. Perryman, M.A.C., Hipparcos and Gaia – the Development of Space Astrometry in Europe, 2004, IAC Winter School 2003, (Accepted for Publication). Perryman, M.A.C., Our Galaxy in Three-Dimensions – the Jeremiah Horrocks Memorial Lecture, 2004, Transit of Venus – New Views of the Solar System and Galaxy, IAU Coll 196, (Accepted for Publication). Sanz-Forcada, J., Dupree, A.K., Active Stars and He I 10830 A, the EUV Connection, 2004, High Resolution Infrared Spectroscopy in Astronomy, (Accepted for Publication). Sanz-Forcada, J., Favata, F., Micela, G., The not-soMAD coronal abundances of active stars, 2004, Chemical Abundances and Mixing in Stars in the Milky Way and its Satellites, (Accepted for Publication). Sanz-Forcada, J., Favata, F., Micela, G., The not-soMAD coronal abundances of active stars, 2004, 13th Cambridge Workshop on Cool Stars, (Accepted for Publication). Sciortino, S., Micela, G., Favata, F., Giardino, G., Flaccomio, E., Damiani, F., X-ray Observations of Star Formation Regions – EPIC results in L1551 and Upper Sco-Cen, 2004, Mem. S. A. It., 75, 428. Sidoli, L., Parmar, A.N., Oosterbroek, T., XMM-Newton results on the ultracompact low-mass X-ray binary 4U 1850-087 in the globular cluster NGC 6712, 2004, The 5th INTEGRAL Workshop – The INTEGRAL Universe, ESA SP-552, 389. Sidoli, L., Parmar, A.N., Oosterbroek, T., The First Broad-Band Persistent X-ray Spectrum of the Dipping Low Mass X-ray Binary EXO 0748-676, 2004, The 5th INTEGRAL Workshop – The INTEGRAL Universe, ESA SP-552, 385. Tauber, J., Prospects for Polarimetry of the Interstellar Medium with the Planck Satellite, 2004, The Magnetized Interstellar Medium, 191. Tielens, A.G.G.M., Peeters, E., Bakes, E.L.O., Spoon, H.W.W., Hony, S., PAHs and Star Formation, 2004, sec4.qxd 7/12/05 9:52 AM Page 120 120 ASP Conf. Ser. 323: Star Formation in the Interstellar Medium Workshop, in Honor of David Hollenbach, Chris McKee and Frank Shu. Walter, R., Courvoisier, T.J.-L., Foschini, L., Lebrun, F., Lund, N., Parmar, A., Rodiguez, J., Tomsock, J.A., Ubertini, P., IGR J16318-4848 & CO – A new population of hidden high mass X-ray binaries in the Norma arm of the Galaxy, 2004, Proc. 5th INTEGRAL Workshop, ESA SP-552, 417. publications Planetary Missions Division Refereed Journals, 2003 Arpigny, C., Jehin, E., Manfroid, J., Hutsemekers, D., Schulz, R., Stuewe, J.A., Zucconi, J.-M., Ilyin, I., Anomalous nitrogen isotope ratio in comets – possible connection with interplanetary dust particles and organic molecules, 2003, Science, 301, 1522-1524. Clausen, K.C., Hassan, H., Verdant, M., Couzin, P., Huttin, G., Brisson, M., Sollazzo, C., Lebreton, J.-P., The Huygens Probe System Design, 2003, Space Sci. Rev., Special Cassini/Huygens issue, 35. Heather, D.J., Dunkin, S.K., Geology and Stratigraphy of King Crater, Lunar Farside, 2003, Icarus, 163, 307-329. Heather, D.J., Dunkin, S.K., Wilson, L., Volcanism on the Marius Hills plateau – Observational analyses using Clementine multispectral data, 2003, J. Geophys. Res., 108/E3, 3-1. Kolokolova, L., Lara, L.M., Schulz, R., Stuewe, J.A., Tozzi, G.P., Color of an ensemble of particles with a wide power-law size distribution – application to observations of Comet Hale-Bopp at 3 AU, 2003, J. Quantitative Spectroscopy and Radiative Transfer, 79-80, 861-871. Lebreton, J.-P., Matson, D.L., The Huygens Probe – Science, Payload and Mission, 2003, Space Sci. Rev., Special Cassini/Huygens, 41. Michael, G.G., Coordinate registration by automated crater recognition, 2003, Planet. Space Sci., 51/9-10, 563. Molina-Cuberos, G., Witasse, O., Lebreton, J.-P., Rodrigo, R., Lopez-Moreno, J.J., Meteoric ion in the atmosphere of Mars, 2003, Planet. Space Sci., 51/3, 239-249. Schulz, R., Maximize the Outcome of a Comet Mission, but how?, 2003, Adv. Space Res., (Accepted for Publication). Schulz, R., Stuewe, J.A., Boehnhardt, H., Gaessler, W., Tozzi, G.P., Characterization of STARDUST target comet 81P/Wild 2 from 1996 to 1998, 2003, A&A, 298, 345-352. Trautner, R., Grard, R., Hamelin, M., Detection of Subsurface Ice and Water Deposits on Mars with a Mutual Impedance Probe, 2003, J. Geophys. Res., 108/E10, 8047. Witasse, O., Dutuit, O., Correction to “Prediction of a CO22+ layer in the atmosphere of Mars”, 2003, Geophys. Res. Lett., 30, 12. Planetary Missions Division Proceedings and other Publications, 2003 Aleon, J., Arpigny, C., Robert, F., Jehin, E., Manfroid, J., Hutsemekers, D., Zucconi, J.-M., Schulz, R., Stuewe, J.A., Sangely, L., Chaussidon, M., Marty, B., Engrand, C., Cometary organic macromolecules in interplanetary dust particles?, 2003, Lunar and Planetary Science, XXXIV, 1308. sec4.qxd 7/12/05 9:52 AM Page 121 publications Arpigny, C., Cochran, A.L., Jehin, E., Manfroid, J., Hutsemekers, D., Zucconi, J.-M., Endl, M., Cochran, W.D., Schulz, R., Anomalous 14N/15N ratio in comets 122P/1995 S1 (de Vico) and 153P/2002 C1 (Ikeya-Zhang), 2003, Bull. Am. Astron. Soc., 35/4, 986. Collon, M., Buis, E.J., Beijersbergen, M., Kraft, S., Erd, C., den Hartog, R., Owens, A., Falkner, P., Schulz, R., Peacock, A., Design and performance of the payload instrumentation of the BepiColombo Mercury Planetary Orbiter, 2003, Proceedings of the Fifth IAA International Conference on Low-Cost Planetary Missions, ESA SP-542, 501. Falkner, P., Schulz, R., The BepiColombo Mission to Mercury, 2003, Bull. Am. Astron. Soc., 35/4, 1001. Fulchignoni, M., Ferri, F., Angrilli, F., Bar-Nun, A., Barucci, M.A., Bianchini, G., Borucki, W., Coradini, M., Coustenis, A., Falkner, P., Flamini, E., Grard, R., Hamelin, M., Harri, A.M., Leppelmeier, G.W., LopezMoreno, J.J., McDonnell, J.A.M., McKay, C.P., Neubauer, F.H., Pedersen, A., Picardi, G., Pirronello, V., Rodrigo, R., Schwingenschuh, K., Seiff, A., Svedhem, H., Vanzani, V., Zarnecki, J., The Characterisation of Titan’s Atmospheric Physical Properties by the Huygens Atmospheric Structure Instrument (HASI), 2003, The Cassini-Huygens Mission, 395-431. Kraft, S., Collon, M., Montella, J., Buis, E.J., Beijersbergen, M., Erd, C., Falkner, P., Schulz, R., Peacock, A., On the concepts of a highly integrated payload suite for use in future planetary missions, the example of the BepiColombo Mercury Planetary Orbiter, 2003, Proc. Fifth IAA International Conference on Low-Cost Planetary Missions, ESA SP-542, 219. Schulz, R., Kern, Koma und Schweife, 2003, Sterne & Weltraum Special: Kometen und Asteroiden, 2/03, 2832. Schulz, R., Wirtanen – A short period comet, 2003, CNES Magazine, 18, 34. Schulz, R., Rosetta goes to comet Wirtanen, 2003, The Observatory, 123/1174, 115-118. Schulz, R., Falkner, P., Peacock, A., Erd, C., Rando, N., Kraft, S., The BepiColombo Mission, 2003, Highlights in Astronomy, 13. Schulz, R., Stuewe, J.A., Boehnhardt, H., Postperihelion monitoring of Comet 67P/Churyumov-Gerasimenko, the new Rosetta target, 2003, Bull. Am. Astron. Soc., 35/4, 970. Thomas, N., Schulz, R., Falkner, P., The BepiColombo Lander – MSE, 2003, Highlights in Astronomy, 13. Trautner, R., Chicarro, A.C., Martin, P.D., Coordinated Science Operations of Mars Express Orbiter and Lander, 2003, Lunar and Planetary Science, XXXIV, 1634. Trautner, R., Simoes, F., Grard, R., Hamelin, M., A new instrument for measuring the low frequency electrical properties of planetary subsurface materials, 2003, ESA SP-543, 193. 121 Planetary Missions Division Refereed Journals, 2004 Bolton, S.J., Hansen, C.J., Matson, D.L., Spilker, L.J., Lebreton, J.-P., Cassini/Huygens flyby of the Jovian system, 2004, J. Geophys. Res., 109, 1-5. Campbell-Brown, M.D., Koschny, D., Model of the ablation of faint meteors, 2004, A&A, 418, 751-758. Culot, F., Lathuillere, C., Lilensten, J., Witasse, O., The OI 630.0 and 557.7 nm dayglow measured by WINDII and modeled by TRANSCAR, 2004, Ann. Geophysicae, 22, 1947-1960. Hansen, C.J., Bolton, S.J., Matson, D.L., Spilker, L.J., Lebreton, J.-P., The Cassini-Huygens Flyby of Jupiter, 2004, Icarus, 172, 1-8. Jehin, E., Manfroid, J., Cochran, A.L., Arpigny, C., Zucconi, J.M., Hutsemekers, D., Cochran, W.D., Endl, M., Schulz, R., Anomalous 14N/15N ratio in comets 122P/de Vico) and 153P/Ikeya-Zhang, 2004, ApJ, 613, L161-L164. Kazeminjad, B., Perez-Ayúcar, M., Lebreton, J.-P., Sanchez-Nogales, M., Belló-Mora, M., Strange, N., Roth, D., Popken, L., Clausen, K., Couzin, P., Simulation and analysis of the revised Huygens probe entry and descent trajectory and radio link modelling., 2004, Planet. Space Sci., 52, 799-814. Lara, L.M., Tozzi, G.P., Boehnhardt, H., DiMartino, M., Schulz, R., Gas and dust in comet C/2000 WM1 during its closest approach to Earth. Optical imaging and long-slit spectroscopy, 2004, A&A, 422, 717-729. Lilensten, J., Simon, C., Witasse, O., Dutuit, O., Thissen, R., Alcaraz, C., A fast computation on the diurnal secondary ion production in the ionosphere of Titan, 2004, Icarus, (Accepted for Publication). Lilensten, J., Witasse, O., Simon, C., Soldi-Lose, H., Dutuit, O., Thissen, R., Alcaraz, C., Prediction of a N2++ layer in the upper atmosphere of Titan, 2004, Geophys. Res. Lett., (Accepted for Publication). Michael, G.G., Beagle-2 position determination from the returned camera panoramas using MOLA data, 2004, Planet. Space Sci., 52, 271. Morel, L., Witasse, O., Warnant, R., Cerisier, J.-C., Blelly, P.-L., Lilensten, J., Diagnostic of the dayside ionosphere of Mars using the Total Electron Content Measurement by the Neige/Netlander experiment – an assessment study, 2004, Planet. Space Sci., 52/7, 603611. Schulz, R., Stuewe, J.A., Boehnhardt, H., Rosetta target comet 67P/Churyumov-Gerasimenko. Postperihelion gas and dust prodution rates, 2004, A&A, 422, L19L21. Tozzi, G.P., Lara, L.M., Kolokolova, L., Boehnhardt, H., Licandro, J., Schulz, R., Sublimating components in the Coma of Comet C/2000 WM1 (LINEAR), 2004, A&A, 424, 325-330. sec4.qxd 7/12/05 9:52 AM Page 122 122 Planetary Missions Division Proceedings and other Publications, 2004 DiMartino, M., Battistelli, E., Carbognani, A., Cellino, A., Koschny, D., Resti, A., Tommasi, L., The ‘Smart Panoramic Optical Sensor Head’ – A new Tool for Detecting Luminous Transient Phenomena on Planetary Bodies, 2004, Geophysical Research Abstracts, 6, 02852. Diaz del Rio, J., Koschny, D., Meteor Orbit and Trajectory determination Software (MOTS), 2004, Proc. Int. Meteor Conf., 19-21 Sep 2003, Bollmannsruh, Germany, Int. Met. Org., Berlin, Germany, 23-28. Frew, D., Koschny, D., Harch, A., Planning the commissioning of a multi-payload mission, 2004, Proc. SpaceOps 2004, May 17-21, 2004, Montreal, Canada. Hoofs, R., Koschny, D., van der Plas, P., Planning strategy and supporting tools for the science operations of ESA’s planetary missions, 2004, Proc. SpaceOps 2004, May 17-21, 2004, Montreal, Canada, Canadian Space Agency. Hoofs, R., Titov, D., Svedhem, H., Koschny, D., Ocampo, A., Science Operations Planning for Venus Express, 2004, Geophysical Research Abstracts, 6, 06373. Josset, J.-L., Beauvivre, S., Almeida, M., Barrucci, A., Cerroni, P., Chevrel, S., diSanctis, C., Ehrenfreud, P., Hofmann, B., Josset, M., Koschny, D., Langevin, Y., Mancuso, S., Muinonen, M., Pinet, P., Plancke, P., Shevch, V., Shkuratov, Y., Sodnik, Z., First results from the Smart-1 AMIE Multi-Colour Micro-Camera, 2004, Geophysical Research Abstracts, 6, 07866. Koschny, D., Comparing two potential meteor cameras – the Mintron and the Watec 120N, 2004, Proc. Int. Meteor Conf., 19-21 Sep 2003, Bollmannsruh, Germany, Int. Met. Org., Berlin, Germany, 59, 63. 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An Overview, 2004, Proc., ESA SP-1278, 229242. publications Lebreton, J.-P., Sollazzo, C., Blancquaert, T., Witasse, O., Maize, E., Matson, D.L., Mitchell, R., Spilker, L., Flamini, E., Talevi, M., [and the Huygens Mission Team], High Ambitions for an Outstanding Planetary Mission. Cassini-Huygens, 2004, ESA Bulletin, 120, 11-21. Lebreton, J.-P., Matson, D., The Huygens Mission to Titan. Overview and Status, 2004, Proc. Planetary Probe Atmospheric Entry and Descent Trajectory Analysis and Science, ESA SP-544, 21-30. Matson, D.L., Lebreton, J.-P., Spilker, L.J., The CassiniHuygens mission to the Saturnian system, 2004, Proc., ESA SP-1278, 242/I-242/XVi. Rohner, U., Benz, W., Whitby, J.A., Wurz, P., Schulz, R., Romstedt, J., Miniaturised Time-of-Flight Mass Spectrometer, 2004, Proceedings of the 37th ESLAB Symposium ‘Tools and Technologies for Future Planetary Exploration’, ESA SP-543, 131. Schulz, R., BepiColombo. Visit to Mercury, 2004, ERCA, From indoor air pollution to the search for Earth-like planets in the cosmos, J. de Physique IV Proc., EDP Sciences, 6, 249. Schulz, R., The Mercury Planetary Orbiter of BepiColombo, 2004, Geophysical Research Abstracts, 6, 04807. Schulz, R., Anomalous Nitrogen Isotopic Ratio in Comets, 2004, ESA Space Science News, 6, 8-9. Schulz, R., Comet 67P/Churyumov-Gerasimenko, the new Rosetta Target, 2004, CNES Magazine, February 2004, 18. Schulz, R., Stuewe, J.A., Boehnhardt, H., Monitoring comet 67P/Churyumov-Gerasimenko from ESO in 2003, 2004, The New Rosetta Targets. Observation, simulations and instrument performances, Kluwer Academic Publishers, Dordrecht, The Netherlands, 15-24. Simões, F., Trautner, R., Grard, R., Hamelin, M., The dielectric properties of Martian Soil Simulant JSC Mars-1 in the frequency range from 20 Hz to 10kHz, 2004, Lunar and Planetary Conference, XXXIV, 205. Svedhem, H., Lebreton, J.-P., Zarnecki, J., Hathi, B., Using Speed of Sound Measurements to Constrain the Huygens Probe Descent Profile, 2004, Int. Workshop ‘Planetary Probe Atmospheric Entry and Descent Trajectory Analysis and Science’, Lisbon, Portugal, 69 October 2003, ESA SP-544, 221-228. Trautner, R., Bello-Mora, M., Hechler, M., Koschny, D., A new celestial navigation method for Mars landers, 2004, Lunar and Planetary Science, XXXV, 1106. Trautner, R., Koschny, D., A new Application for Planetary Lander Cameras – Lander Position and Attitude Determination using Night Sky Images, 2004, Geophysical Research Abstracts, 6, 03614. Trautner, R., Manaud, N., Michael, G., Griffiths, A., Beauvivre, S., Koschny, D., Coates, A., Josset, J., Determination of the Beagle2 landing site, 2004, ESA SP-544, 175. Wirth, K.R., Hoofs, R., Koschny, D., Frew, D., Dhiri, V., Rosetta Science Mission Overview, 2004, 35th sec4.qxd 7/12/05 9:52 AM Page 123 publications COSPAR Scientific Assembly, Paris, France, 18-25 July 2004. Wirth, K.R., Zender, J., Arviset, C., PSA ready to deliver science data from ESA planetary missions, 2004, EGU 1st General Assembly, Geophysical Research Abstracts, 6, 01467. Zender, J., Witasse, O., Koschny, D., Campbell-Brown, M., Diaz del Rio, J., Trautner, R., Knöfel, A., Meteor spectroscopy – Introduction to theory, setup, and data analysis, 2004, Proc. Int. Met. Conf. 2003, 19-21 Sep 2003, Bollmannsruh, Germany, 168. Zender, J.J., Schwehm, G., Arviset, C., The Planetary Science Archive, Introduction and Overview, 2004, Ensuring the long-term Preservation and Adding Value to the Scientific and Technical Data, Proceedings, ESA WPP-232, 31-38. Zender, J.J., Schwehm, G., Wilke, M., The ROSETTA Video Approach, An Overview and Lessons Learned so far, 2004, Proc. 55th International Astronautical Congress, Zarm, Univ. Bremen, Germany (CD). 123 Science Operations and Data Systems Division Refereed Journals, 2003 Barret, D., Olive, J.F., Oosterbroek, T., Simultaneous BeppoSAX and Rossi X-ray Timing Explorer observations of 4U 1812-12, 2003, A&A, 400, 643. Brandt, S. Budtz-Jorgensen, C., Lund, N., Rasmussen, L.L., Laursen, S., Chenevez, J., Westergaard, N.J., Juchnikowski, G., Walter, R., Schmidt, M., Much, R., X-ray observation of the Crab Pulsar and Nebula with JEM-X on INTEGRAL, 2003, A&A, 411, L433. 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International Lunar Conference 2003, A.A.S./Space Age Publ. (Ed. S.M. Durst et al.), 213. Zegers, T.E., Conan, Y.G., Foing, B.H., Noachian Martian highlands; the habitat of ancient life?, 2004, Proc. Third European Workshop on Exo-Astrobiology, 18-20 November 2003, Madrid, Spain, ESA SP-545, 313. Zegers, T.E., Conan, Y.G., Foing, B.H., Geology of Noachian Martian Highlands Surrounding the Gusev Crater, 2004, 35th Lunar and Planetary Science Conference, March 15-19, 2004, League City, Texas, LPI, 1767. sec4.qxd 7/12/05 9:52 AM Page 143 publications Science Payload and Advanced Concepts Office Refereed Journals, 2003 Acker, A., Neiner, C., Quantitative classification of WR nuclei of planetary nebulae, 2003, A&A, 403, 659. Bertuccio, G., Casiraghi, R., Maiocchi, D., Owens, A., Bavdaz, M., Peacock, A., Andersson, H., Nenonen, S., Noise Analysis of Gallium Arsenide Pixel X-Ray Detectors Coupled to Ultra-Low Noise Electronics, 2003, IEEE Trans. Nucl. Sci., 50, 723. Brammertz, G., Kozorezov, A.G., Wigmore, J.K., Hartog, R. den, Verhoeve, P., Martin, D., Peacock, A., Golubov, A.A., Rogalla, H., Energy-dependent kinetic model of photon absorption by superconducting tunnel junctions, 2003, J. Appl. Phys, 94, 5854. Ellery, A., Kolb, C., Lammer, H., Parnell, J., Edwards, H., Richter, L., Patel, M., Romstedt, J., Dickensheets, D., Steele, A., Cockell, C., Astrobiological instrumentation for Mars – the only way is down, 2003, International J. Astrobiology, 1, 365-380. Gondoin, P., The corona of V390 Aurigae (HD 33798), 2003, A&A, 355, 364. Gondoin, P., The corona of HD 223460 (HR 9024), 2003, A&A, 409, 263. Gondoin, P., Orr, A., Lumb, D., XMM-Newton observation of the Seyfert 1 galaxy ESO 141-G55, 2003, A&A, 398, 967. Gondoin, P., Orr, A., Lumb, D., Siddiqui, H., XMMNewton observation of the Seyfert 1 galaxy NGC 3227, 2003, A&A, 397, 883. Gostilo, V., Owens, A., Bavdaz, M., Lisjutin, I., Peacock, A., Sipila, H., Zatoloka, S., A comparison of the X-ray performance of TlBr crystals grown by the Bridgeman–Stockbarger and travelling molten zone methods, 2003, Nucl. Instr. & Meth., A509, 47. Lumb, D.H., Finoguenov, A., Saxton, R., Aschenbach, B., Gondoin, P., Kirsch, M., Stewart, I., In-orbit Vignetting Calibrations of XMM-Newton Telescopes, 2003, Experimental Astronomy, 15, 89. Lumb, D.H., Rando, R., Peacock, A., Favata, F., Perryman, M.A.C., Focal plane cameras for ESA optical astronomy missions, 2003, Nucl. Instr. & Meth., A513, 112. Neiner, C., Geers, V.C., Henrichs, H.F., Floquet, M., Fremat, Y., Hubert, A.-M., Preuss, O., Wiersema, K., Discovery of a magnetic field in the Slowly Pulsating B star zeta Cassiopeia, 2003, A&A, 406, 1019. Neiner, C., Henrichs, H.F., Floquet, M., Fremat, Y., Preuss, O., Hubert, A.M., Geers, V.C., Tijani, A.H., Nichols, J., Jankov, S., Rotation, pulsations and magnetic field in V2052 Ophiuchi – a new He-strong star, 2003, A&A, 411, 565. Neiner, C., Hubert, A.-M., Fremat, Y., Floquet, M., Jankov, S., Preuss, O., Henrichs, H.F., Zorec, J., Rotation and magnetic field in the Be star omega Orionis, 2003, A&A, 409, 275. Neumann, D.M., Lumb, D.H., Pratt, G.W., Briel, U.G., The dynamical state of the Coma cluster with XMMNewton, 2003, A&A, 400, 811. 143 Nevalainen, J., Lieu, R., Bonamente, M., Lumb, D., Soft X-Ray Excess Emission in Clusters of Galaxies Observed with XMM-Newton, 2003, ApJ, 584, 716. Owens, A., Bavdaz, M., Brammertz, G., Gostilo, V., Graafsma, H., Kozorezov, A., Krumrey, M., Lisjutin, I., Peacock, A., Puig, A., Sipila, H., Zatokola, S., The X-ray response of TlBr, 2003, Nucl. Instr. & Meth. A, A497, 370. Owens, A., Bavdaz, M., Brammertz, G., Gostilo, V., Haack, N., Kozorezov, A., Lisjutin, I., Peacock, A., Zatoloka, S., Hard X-ray spectroscopy using a small format TlBr array, 2003, Nucl. Instr. & Meth. A, A497, 359. Owens, A., Mosselmans, J., Peacock, A., Near K-edge linear attenuation coefficients for amorphous and crystalline GaAs, 2003, J. Radiation Physics and Chemistry, 66, 1. Reynolds, A.P., Bruijne, J.H.J. de, Perryman, M.A.C., Peacock, A., Bridge, C.M., Temperature determination via STJ optical spectroscopy, 2003, A&A, 400, 1209-1217. Verhoeve, P., Brammertz, G., Martin, D., Peacock, A., Quasiparticle loss rates in Ta-based superconducting tunnel junctions, 2003, Nucl. Instr. & Meth., 520, 246. Verhoeve, P., Martin, D., Dordrecht, A. van, Verveer, J., Hartog, R. den, Peacock, A., 120-pixel array of superconducting tunnel junctions as spectro-photometer for optical astronomy, 2003, Nucl. Instr. & Meth., 513, 206. Science Payload and Advanced Concepts Office Proceedings and other Publications, 2003 Absil, O., den Hartog, R., Erd, C., Gondoin, P., Kaltenegger, L., Fridlund, M., Rando, N., Wilhelm, R., GENIESIM – The GENIE Simulation Software, 2003, Proc. ‘Towards other Earths’, ESA SP-539, 317. Atzei, A.C., Falkner, P., Berg, M.L. van den, Peacock, A., Jupiter Microsat Explorer Programme, 2003, 5th IAA Conference on Low-Cost Planetary Missions, ESA SP-542, 189. Atzei, A.C., Falkner, P., Berg, M.L. van den, Peacock, A., The Jupiter Microsat Explorer Programme, 2003, 37th ESLAB Symp., 2-4 December 2003, ESA SP-543, 17. Bavdaz, M., Peacock, A., X-ray Optics – new technologies at ESA, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Telescopes and Instruments for Astronomy, 4851, 421. Bavdaz, M., Peacock, A., Laan, T. van der, Parmar, A., The XEUS – approaches to mission design, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Telescopes and Instruments for Astronomy, 4851, 396. Berg, M.L. van den, Falkner, P., Atzei, A.C., Peacock, A., Venus Microsat Explorer Programme, an ESA Technology Reference Mission, 2003, Proc. 5th IAA conference on low-cost planetary missions, ESA SP-542, 73. sec4.qxd 7/12/05 9:52 AM Page 144 144 Bertrand, R., Del Bianco, A., Harnisch, B., Jessberger, E.K., Peuser, P., Romstedt, J., Rost, D., Schneider, K., Weber, I., A minituarized laser instrument for chemical and mineralogical in-situ analysis on planetary surfaces, 2003, Geophysical Research Abstracts, 5, EAE03-A-05861. Erd, C., Owens, A., Brammertz, G., Lumb, D., Bavdaz, M., Peacock, A., Nenonen, S., Andersson, H., Measurements of the quantum efficiency and depletion depth in gallium-arsenide detectors, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Detectors and Applications IV, 4784, 386. Falkner, P., Erd, C., Highly Integrated Payload Suites and Related Data Link Requirements, 2003, ISWS – International SpaceWire Seminar 2003, 1, 25. Falkner, P., Erd, C., Kraft, S., Peacock, T., Remote Sensing Instrument Suite for Planetary Exploration, 2003, Geophysical Research Abstracts, 5, 12462. Falkner, P., Romstedt, J., Verhoeve, P., Peacock, A., Instrumentation for in-situ measurements on the surface of Mercury, 2003, Geophysical Research Abstracts, 5, 12557. Fridlund, M., Gondoin, P., The Darwin Mission, 2003, SPIE Proceedings – Interferometry in Space, 4852, 394. Gondoin, P., Absil, O., Fridlund, M., Erd, C., Hartog, R. den, Rando, N., Glindemann, A., Koehler, B., Wilhelm, R., Karlsson, A., Labadie, L., Mann, I., Peacock, A., Richichi, A., Sodnik, Z., Tarenghi, M., Volonte, S., The Darwin Ground-based European Nulling Interferometry Experiment (GENIE), 2003, SPIE Proceedings – Interferometry for Optical Astronomy II, 4838, 700. Gondoin, P., Absil, O., den Hartog, R., Kaltenegger, L., Eiroa, C., Erd, C., Fridlund, M., Karlsson, A., Peacock, A., Sodnik, Z., Volonte, S., Wilhelm, R., Schoeller, M., Glindemann, A., The Ground-based European Nulling Interferometry Experiment (Darwin-GENIE), 2003, Proc. ‘Towards Other Earths’, ESA SP-539, 121. Gondoin, P. XMM-Newton observation of the Seyfert 1 galaxy IC4329A, 2003, Active Galactic Nuclei: from Central Engine to Host Galaxy, ASP Conf. Series 290, 97. Grard, R., Falkner, P., The Bepi Colombo Mission to Mercury, 2003, Geophysical Research Abstracts, 5, 10727. Hartog, R. den, Absil, O., Kaltenegger, L., Gondoin, P., Wilhelm, R., Fridlund, M., Could GENIE detect Hot Jupiters?, 2003, Proc. ‘Towards Other Earths’, ESA SP-539, 399. Hartog, R. den, Kozorezov, A., Verhoeve, P., Martin, D., Noise in a Quatratran-based detector – a comparison with Superconducting Tunnel Junctions, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Telescopes and Instruments for Astronomy, 4851, 1002. Hartog, R. den, Owens, A., Kozorezov, A., Bavdaz, M., Peacock, A., Gostilo, V., Lisjutin, I., Zatoloka, S., Optimization of array design for TlBr imaging publications detectors, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Telescopes and Instruments for Astronomy, 4851, 922. Martin, D., Verhoeve, P., Hartog, R. den , Bruijne, J. de, Reynolds, A., Dordrecht, A. van, Verveer, J., Peacock, A., 12x10 pixels superconducting tunnel junction array based spectrophotometer for optical astronomy, 2003, SPIE Proceedings – Instrument Design and Performance for Optical/Infrared Ground-based Telescopes, 4841, 805. Miyaji, T., Griffiths, R.E., Lumb, D., Sarajedini, V., Siddiqui, H., XMM-Newton view of the Hubble Deep Field-North and Groth-Westphal strip regions, 2003, Astron. Nachtrichten, 324, 24. Neiner, C., Appourchaux, T., Global fitting of power spectra of solar-like stars, 2003, 2nd Eddington Workshop: Stellar structure and habitable planet finding, ESA SP-538, 373. Neiner, C., Hubert, A.-M., Floquet, M., Seismology of Be stars, 2003, 2nd Eddington Workshop: Stellar structure and habitable planet finding, ESA SP-538, 369. Owens, A., Peacock, A., Bavdaz, M., Progress in Compound Semiconductors, 2003, SPIE Proceedings – X-Ray and Gamma-Ray Telescopes and Instruments for Astronomy, 4851, 1059. Rando, N., Murphy, E., Falkner, P., Peacock, A., The Laser Altimeter for Planetary Exploration (LAPE), 2003, Geophysical Research Abstracts, 5, 12399. Torkar, K., Riedler, W., Romstedt, J., Jeszensky, H., Steller, M., Arends, H., The MIDAS atomic force microscope for cometary dust – technical highlights and future perspectives, 2003, Geophysical Research Abstracts, 5, EAE-A-07246. Verhoeve, P., Hartog, R. den, Kozorezov, A., Martin, D., Dordrecht, A. van, Wigmore, J.K., Peacock, A., Integration time dependence of tunnel noise and energy resolution of superconducting tunnel junctions, 2003, SPIE Proceedings – Instrument Design and Performance for Optical/Infrared Ground-based Telescopes, 4841, 141. Science Payload and Advanced Concepts Office Refereed Journals, 2004 Brammertz, G., Peacock, A., Verhoeve, P., Martin, D., Venn, R., Optical photon detection in Al Superconducting Tunnel Junctions, 2004, Nucl. Instr. & Meth., A 520, 508. Gondoin, P., X-ray spectroscopy of the W UMa-type binary 44 Bootis, 2004, A&A, 426, 1035. Gondoin, P., The corona of HD 199178 (V 1794 Cygni), 2004, A&A, 413, 1095. Gondoin, P., X-ray spectroscopy of the W UMa-type binary VW Cephei, 2004, A&A, 415, 1113. Gondoin, P., Orr, A., Siddiqui, H., XMM-Newton observations of the dwarf elliptical galaxy NGC 3226, 2004, A&A, 420, 905. sec4.qxd 7/12/05 9:52 AM Page 145 publications Kozorezov, A., Wigmore, K., Owens, A., den Hartog, R., Peacock, A., The effect of carrier diffusion on the characteristics of semiconductor imaging arrays, 2004, Nucl. Instr. & Meth., A531, 52. Lumb, D.H., Bartlett, J.G., Romer, A.K., Blanchard, A., Burke, D.J., Collins, C.A., Nichol, R.C., Giard, M., Marty, P., Nevalainen, J., Sadat, R., Vauclair, S., The XMM-NEWTON Omega Project – I. The X-ray Luminosity-Temperature Relation at z>0.4, 2004, A&A, 420, 383. Martin, D.D.E., Peacock, A., Verhoeve, P., FernandezLeon, A., Glass, B., Maehlum, G., 64-channel preamplifier ASICs for superconducting tunnel junction readout, 2004, Nucl. Instr. & Meth., A 520, 570-573. Martin, D.D.E., Verhoeve, P., Peacock, A., Dordrecht, A. van, Verveer, J., Hijmering, R., A 12x10 pixels superconducting tunnel junction array based spectrophotometer for optical astronomy, 2004, Nucl. Instr. & Meth., A 520, 512-515. Owens, A., XANES fingerprinting – a technique for investigating CCD surface structures and measuring dead layer thicknesses, 2004, Nucl. Instr. & Meth., A526, 391. Owens, A., Peacock, A., Compound Semiconductor Radiation Detectors, 2004, Nucl. Instr. & Meth., A513, 18. Rando, N., Lumb, D., Bavdaz, M., Martin, D., Peacock, A., Space science applications of cryogenic detectors, 2004, Nucl. Instr. & Meth., A-522, 62. Scelsi, L., Maggio, A., Peres, G., Gondoin, P., X-ray spectroscopy of the Hertzsprung-gap giant 31 Com, observed with XMM-Newton, 2004, A&A, 413, 643. Vaitkus, J., Gostilo, V., Jasinskaite, R., Mekys, A., Owens, A., Tamosiunas, S., Zatoloka, S., Zindulis, A., Investigation of Degradation of Electrical and Photoelectrical Properties in TlBr Crystals, 2004, Nucl. Instr. & Meth., A531, 192. Science Payload and Advanced Concepts Office Proceedings and other Publications, 2004 Absil, O., Hartog, R. den, Gondoin, P., Fabry, P., D’Arcio, L., Wilhelm, R., Gitton, P., Puech, F., Influence of atmospheric turbulence on the performance and design of GENIE, 2004, Proc. SPIE Conference 2004 Glasgow, Astronomical Telescopes & Instrumentation, 5491, 1257. Atzei, A.C., Falkner, P., Berg, M.L. van den, Peacock, A., The Jupiter Minisat Explorer – A Technology Reference Mission, 2004, Proceedings of 37th ESLAB Symposium, ESA SP 543, 17. Bavdaz, M., Lumb, D., Peacock, A., Beijersbergen, M., Kraft, S., Development of X-ray optics for the XEUS Mission, 2004, Proceedings SPIE, 5539, 104. Bavdaz, M., Lumb, D.H., Peacock, A., XEUS Mission Reference Design, 2004, Proceedings SPIE, 5488, 530. Bavdaz, M., Lumb, D.H., Peacock, A., Beijersbergen, 145 M., Kraft, S., Status of X-ray Optics Development for the XEUS Mission, 2004, Proceedings SPIE, 5488, 829. Bavdaz, M., Peacock, A., Tomaselli, E., Beijersbergen, M., Collon, M., Flyckt, E., Fairbend, R., Boutot, J.-P., Progress at ESA on High Energy Optics Technologies, 2004, SPIE Proceedings, 5168, 136. Beijersbergen, M., Kraft, S., Bavdaz, M., Lumb, D., Guenther, R., Collon, M., Mieremet, A., Fairbend, R., Peacock, A., Development of X-ray pore optics novel high-resolution silicon millipore optics for XEUS and ultralow mass glass micropore optics for imaging and timing, 2004, Proceedings SPIE, 5539, 104. Beijersbergen, M., Kraft, S., Gunther, R., Mieremet, A., Collon, M., Bavdaz, M., Lumb, D.H., Peacock, A., Silicon Pore Optics – novel lightweight highresolution X-ray optics developed for XEUS, 2004, Proceedings SPIE, 5488, 868. Berg, M.L. van den, Falkner, P., Atzei, A.C., Peacock, A., Venus MicroSat Explorer Programme, an ESA Technology Reference Mission, 2004, Proc. Workshop on Planetary Probe Atmosphric Entry and Descent Trajectory Anaylsis and Science, ESA SP-544, 275. Berg, M.L. van den, Falkner, P., Atzei, A.C., Peacock, A., Venus Entry Probe, an ESA Technology Reference Mission, 2004, Tool and Technologies for future planetary exploration, Proc. 37th ESLAB Symposium, 2-4 December 2003, ESA SP-543, 23. Brammertz, G., Verhoeve, P., Martin, D., Peacock, A., Venn, R., Future optical detectors based on Al superconducting tunnel junctions, 2004, Proceedings SPIE, 5499, 269. D’Arcio, L.A., Karlsson, A., Search for Extraterrestrial Planets – The DARWIN Mission, 2004, Proc. 5th International Conference on Space Optics – ICSO 2004, ESA SP-554, 213. D’Arcio, L.A., Karlsson, A., Gondoin, P., Use of OPD modulation techniques in stellar interferometry, 2004, SPIE Proceedings New frontiers in stellar interferometry, 5491, 851. Falkner, P., ESA’s Technology Reference Studies, 2004, 8th ESA Workshop on Advanced Space Technologies for Robotics and Automation, ‘ASTRA 2004’, 8, 155. Falkner, P., Atzei, A., van den Berg, M., Schiele, A., Microprobes for in-situ measurements on Planetray surfaces and Atmospheres, 2004, Geophysical Research Abstracts, 6, 5458. Falkner, P., Erd, C., Kraft, S., Highly Integrated Payload Suites for Planetary Exploration, 2004, Geophysical Research Abstracts, 6, 6241. Falkner, P., Rando, N., Murphy, E., Update on Laser Altimeters for Planetary Exploration, 2004, Geophysical Research Abstracts, 6, 05450. Gondoin, P., Absil, O., Hartog, R. den, Wilhelm, R., Gitton, P., D’Arcio, L., Fabry, P., Puech, F., Fridlund, M., Schoeller, M., Glindemann, A., Bakker, E., Karlsson, A., Peacock, A., Volonte, S., Paresce, F., Richichi, A., Darwin-GENIE: a nulling instrument at sec4.qxd 7/12/05 9:52 AM Page 146 146 the VLTI, 2004, Proc. SPIE Conference 2004 Glasgow, Astronomical Telescopes & Instrumentation, 5491, 775. Hartog, R. den, Absil, O., Gondoin, P., D’Arcio, L., Fabry, P., Kaltenegger, L., Wilhelm, R., Gitton, P., Puech, F., Fridlund, M., The simulated detection of low-mass companions with GENIE, 2004, Proc. SPIE, New Frontiers in Stellar Interferometry, 5491, 160. Hughes, G.W., Macdonald, M., McInnes, C.R., Atzei, A., Falkner, P., Analysis of a Solar Sail Mercury Sample Return Mission, 2004, Proceedings IAC, Vancouver 2004, CDROM. Jones, L.R., Maughan, B.J., Ebeling, H., Scharf, C., Perlman, E., Lumb, D., Gondoin, P., Mason, K.O., Cordova, F., Priedhorsky, W.C., An XMM and Chandra view of massive clusters of galaxies to z=1, 2004, Clusters of Galaxies: Probes of Cosmological Structure and Galaxy Evolution, Carnegie Observatories Astrophysics Series, Pasadena, California, USA, 25. Kaltenegger, L., Karlsson, A., Requirements on the stellar rejection for the DARWIN mission, 2004, Proceedings SPIE, Glasgow, Astronomical Telescopes & Instrumentation, 5491, 275. Karlsson, A., Wallner, O., Perdigues Armengol, J., Absil, O., Three Telescope Nuller, based on multi beam injection into single mode waveguide, 2004, SPIE – Astronomical Telescopes, Glasgow 2004, 5491, 831. Kilter, M., Micropropulsion Assessment for DARWIN, 2004, Micropropulsion Assessment for DARWIN, 5.2, 145. Kilter, M., Karlsson, A., Micropropulsion Technologies for the European high-precision Formation Flying Interferometer DARWIN, 2004, Proc. 4th International Spacecraft Propulsion Conference, ESA SP-555, 85. Lumb, D.H., Instrumentation Package for ESAs (XEUS) X-ray Early Universe Spectroscopy Mission, 2004, Proceedings SPIE, 5165, 1. Lumb, D.H., XEUS Mission – Detector Spacecraft Instrumentation Package, 2004, Proceedings SPIE, 5488, 539. Lyngvi, A., Falkner, P., Atzei, A., Renton, D., van den Berg, M.L., Peacock, A., ESA’s Technology Reference Studies, 2004, Proceedings IAC, Vanouver 2004, IAC, IAC-04-U.1.06. Lyngvi, A., Falkner, P., Peacock, A., The Interstellar Heliopause Probe, 2004, Proceedings of Tools and Technologies for Future Planetary Exploration, 37th ESLAB Symposium, ESA SP-543, 11-17. Lyngvi, A., Falkner, P., Peacock, A., The Interstellar Heliopause Probe, 2004, Proceedings IAC, Vancover 2004, paper number IAC-04-Q.2.A.06. Owens, A., Alha, L., Andersson, H., Bavdaz, M., Brammertz, G., Helariutta, K., Peacock, A., Ldmsd, V., Nenonen, S., The effects of proton induced radiation damage on compound semiconductor X-ray detectors, 2004, SPIE, 5501, 403. publications Owens, A., Andersson, H., Campbell, M., Lumb, D., Nenonen, S., Tlustos, L., GaAs arrays for X-ray spectroscopy, 2004, SPIE, 5501, 241. Renton, D.C., Falkner, P., Peacock, A., Deimos Sample Return Technology Reference Mission, 2004, Proc. ‘Tools and Technologies for Future Planetary Exploration’, 37th ESLAB Symposium, ESA SP-543, 3. Romstedt, J., Torkar, K., Riedler, W., Jeszenszky, H., Arends, H., Butler, B., Biezen, J. van der, Steller, M., MIDAS – First Results from Rosetta’s Commissioning Phase, 2004, Geophysical Research Abstracts, 6, EGU04-A-01202. Stankov, A., Favata, F., Characterization of the field population in the Pleiades cluster region for EDDINGTON, 2004, Proc. 2nd Eddington workshop: Stellar structure and habitable planet finding, ESA SP-538, 425. Verhoeve, P., Martin, D., Brammertz, G., Hijmering, R., Peacock, A., Photon Counting Cryogenic detectors for Ground-based and Space Telescopes, 2004, Proc. 5th International Conference on Space Optics (ICSO 2004), ESA SP-554, 781. Wallner, O., Perdigues Armengol, J.M., Karlsson, A., Multi-Axial Single-Mode Beam Combiner, 2004, SPIE, Glasgow, 2004, 5491, 798. sec4.qxd 7/12/05 9:52 AM Page 147 publications Stagiaire Research Reports and Theses, 2003 Civeit, T. (Observatoire de Meudon, DESS Outils et Systemes de l’astronomie et de l’espace), Measurement of zonal winds velocity in Titan’s stratosphere with VLT/UVES observations, RSSD supervisor O. Witasse. Coia, D. (Univ. Coll. Dublin), Infrared Observations of Clusters of Galaxies, Ph.D. Thesis, Faculty of Science, National University of Ireland, RSSD co-supervisor L. Metcalfe (with Prof. B. McBreen at U.C.D.). Cordonnier, R. VILSPA RSSD Network Statistics Tool Stage Report, RSSD supervisor C. Arviset. Malloreau, S. (Observatoire de Meudon, DESS Outils et Systemes de l’astronomie et de l’espace), Huygens radar data analysis and test campaign preparation, RSSD supervisor J.-P. Lebreton. Sierra, M. (Spanish Trainee), Extended Source Analysis with the RGS aboard XMM-Newton, RSSD supervisor A. Pollock. Sierra, M. (Spanish Trainee), The Use of SNRs as Contamination Monitors for the RGS aboard XMMNewton, RSSD supervisor A. Pollock. Stagiaire Research Reports and Theses, 2004 Aguardo, D. (U. Complutense Madrid), Refinement of the EPIC count rate estimation in PHS tools, Practices at ESAC report, Faculty of Mathematics, RSSD supervisor M. Kirsch, co-supervisor A.I. Gomez de Castro at UCM (Universidad Complutense de Madrid). Barbarisi, I. VOSpec: a Tool to display and superimpose spectra from VO compatible Spectra Server, RSSD supervisor C. Arviset. Brooks Pollock, E. (University College London), Simultaneous Analysis of Galaxy Clusters with the RGS and EPIC Instruments aboard XMM-Newton, RSSD supervisor A. Pollock. Carter, J. (YGT), Review of the XMM-Newton SAS Online Guides and Online Support Structure, RSSD supervisor A. Pollock. Carter, J. (YGT), Order Separation and PI Selection Regions in the Analysis of XMM-Newton RGS data, RSSD supervisor A. Pollock. Couturier-Doux, S. (DESS Outils et Systemes de l’astronomie et de l’espace, Paris-Meudon), Contribution to the operations planning & software tests for the Camera onboard the SMART-1 Mission, RSSD supervisor B.H. Foing. Esquej, M.P. (U. Complutense Madrid), Energy calibration verification of the EPIC cameras with SNR observations, Practices at ESAC report, Faculty of Physical Sciences, Astrophysics and Atmosphere Sciences department, RSSD supervisor M. Kirsch, co-supervisor J. Zamorano at UCM (Universidad Complutense de Madrid). Jimenez-Bailon, E. (U. Autonoma de Madrid), Star 147 Formation in Low Luminosity Active Galactic Nuclei, 2004, Ph.D. Thesis report, published January 2004, defended March 2004. 1999-2003, RSSD supervisor M.Santos-Lleo, co-supervisor: M. Mas-Hesse at LAEFF-INTA, Spain. Jimenez-Esteban, F.M. An Infrared Study of Galactic OH/IR Stars, Ph.D. Thesis, June 2004, RSSD supervisor P. Garcia-Lario, co-supervisor D. Engels at Hamburg Observatory. Jiménez Luján, F. (U. Complutense de Madrid), Análisis de datos de XMM-Newton de galaxias espirales cercanas: Fuentes de rayos X y emisión extensa de M83, September 2004 ‘XMM-Newton data analysis of nearby spiral galaxies: X-ray sources and extended emission in M83’, Practices at ESAC report, Faculty of Physical Sciences, Astrophysics and Atmosphere Sciences department, RSSD supervisor M. Ehle, co-supervisor J. Zamorano at UCM (Universidad Complutense de Madrid). Leyder, J.-C. (Université de Liège), Analysis of Messenger – The NASA mission to Mercury, May 2004, Master Thesis report, Université de Liège, Faculty of Applied Sciences, supervisors ESTEC J. Romstedt, N. Rando, supervisor Univ. Liège, J.-P. Swings. Luna, R. Busqueda de Bandas Difusas en Envolturas Circunestelares, Ph.D. Thesis, November 2004, RSSD supervisor: P. Garcia-Lario, co-supervisor: M.A. Satorre at U. Alcoy. Sarmiento Ares, F. (U. Vigo), System Study of a Planetary Data Handling and Archiving System, State of the Art and Outlook, July 2004, RSSD supervisor J. Zender. Schoenherr, G. (U. Bonn), Scientific X-ray data analysis of the Crab supernova remnant, RSSD supervisor A. Pollock. Seoane Purrinos, L. (U. Vigo), JMAPPS Client-Server Interactive Application for browsing the Mars Surface, RSSD supervisor J. Zender. Simoes, F. (Portuguese trainee), Subsurface Permittivity Probe to detect Water/Ice in Planetary Environments, RSSD supervisors R. Trautner, A. Chicarro, R. Grard. Stebe, A. ESAC Science Archive Team and Computer Support Group WebPortal Improvements Stage Report, RSSD supervisor C. Arviset. Suarez, O. (U. Vigo), Stellar Evolution in the Post-AGB Stage, Ph.D. Thesis, May 2004, RSSD supervisor: P. Garcia-Lario, co-supervisor: M. Manteiga at U. Vigo. Vacher, G. VILSPA Science Archive Team and Computer Support Group WebPortal Design and 1st Implementation Stage Report, RSSD supervisor C. Arviset. van Kan, M. (U. Utrecht), Geologic Evolution of the Gusev Crater region on Mars – using Mars Express, MGS and Mars Odyssey, August 2004, Master Thesis report, Faculty of Earth Sciences Utrecht, RSSD supervisors T. Zegers, B.H. Foing, co-supervisor C.G. Langereis at Utrecht U. sec4.qxd 7/12/05 9:52 AM Page 149 ANNEX 3 Seminars and Colloquia sec4.qxd 7/12/05 9:52 AM Page 150 150 Seminars held at ESTEC 2003 17 January An Observational View on the Variability of Disks around Pre-Main Sequence Stars C. Eiroa, Astronomy Missions Division 31 January NASA’s Far-IR/Submillimeter Roadmap Missions: SAFIR and SPECS D. Leisawitz, NASA Goddard Space Flight Center 14 February Cluster Results and Future Multi-Satellite Mission Concepts H. Laakso, Solar and Heliospheric Missions Division 28 February Luminosity Functions of Young Stellar Clusters T. Prusti, Astronomy Missions Division seminars and colloquia 26 September The Young Earth: A Different Planet T. Zegers, Planetary Missions Division 9 October ALMA – the Atacama Large Millimetre Array W. Wild, SRON 24 October X-ray Emission and Origin of Runaway Stars E. Meurs, Dunsink Observatory 7 November What is XMM Telling us About the Unified Scenario for Active Galactic Nuclei? M. Guinazzi, VILSPA 5 December XMM-Newton Observations of Globular Clusters D. Carrett, CESR 2004 14 March Remote Sensing of Planetary Minerals and Ices by NIR Imaging Spectroscopy, Objects and Methods S. Doute, Laboratoire de Planetologie de Grenoble 28 March The Transition from AGB Stars to Planetary Nebulae as seen by ISO P. Garcia, VILSPA 25 April Measurig the Gas Content of Galaxies: the Effects of a Higher H2 Formation Rate P. Papadopolous, University of Leiden 23 May Optical and Infrared Interferometry A. Quirrenbach, University of Leiden 19 June Measurement of Polarisation of the Cosmic Microwave Background L. Piccirillo, Cardiff University 4 July Halo Gas in Spiral Galaxies F. Fraternali, ASTRON 11 July Venus: Mysteries of the ‘Forgotten Planet’ D.V. Titov, Max Planck Inst. für Aeronomie 12 September Magellan Mission to Venus: What Did we Learn about Venus’ Surface Tectonics and History? P. Rosenblatt, Belgium Royal Observatory 9 January Darwin and Exoplanets: Disks, Exoplanets and Darwin M. Fridlund, Astronomy Missions Division 23 January Early Mission Highlights from the Spitzer Space Telescope A. Marsdon, Astronomy Missions Division 6 February Dust and Gas Content of Quasars and Galaxies in the Early Universe P. Cox, Université Paris Sud 19 February Imaging and Photometry of Mars: Strategy Toward a Multiscale Understanding of the Optical Properties P. Pinet, Observatoire Midi-Pyrenées 19 March Architecture and Concepts for Optical Sensors for Planetary Exploration and Space-Based Astronomy H. Michaelis, DLR 2 April Gas in Elliptical Galaxies and Bulges S. Peletier, University of Groningen 23 April The Great Observatories Origins Deep Survey: First Science Results B. Mobasher, STScI sec4.qxd 7/12/05 9:52 AM Page 151 seminars and colloquia 151 7 May The Origin of Dust at High Redshift L. Dunne, University of Wales Colloquia held at ESTEC 4 June On the Cassini-Huygens Mission J.-P. Lebreton, Planetary Missions Division 9 May The Search for the Complete History of the Cosmos N. Turok, Cambridge University 2 July LISA – A Mission to Detect and Observe Gravitational Waves O. Jennrich, Fundamental Physics Missions Division 21 November Drilling the Chicxulum Dinosaur Killer Crater – How a Meteorite Impact Changed our World J. Smit, Vrije Universitaet 9 July ESO Research Facilities in Chile C. Alloin, ESO 2004 10 September The Pioneer Anomaly: the Data, its Meaning and a Possible Test M.N. Nieto, Los Alamos 7 October Latest Results from Spitzer – An Infrared View of Galaxy Evolution H. Dole, Université Paris Sud 22 October Massive Star Nucleosynthesis in Cygnus X J. Knoedlseder, CESR 5 November The High Resolution Stereo Camera Experiment on Mars Express: First Geoscientific Results R. Jaumann, German Aerospace Centre 12 November Dynamics and Instability in Jupiter’s Outer Magnetosphere D. Southwood, Director of Science 19 November Examples of Studies of the Current Sheet Dynamics by Cluster P. Louarn, CESR 3 December Giant Planets’ Aurora: A Comparative View J.-C. Gerard, Université Liège 2003 5 March The Paradoxes of Evolution: Inevitable Humans but in a Lonely Universe S. Conway-Morris, Cambridge University 18 June Archeoastronomy: Stonehenge and Beyond C. Ruggles, Leicester University sec4.qxd 7/12/05 9:52 AM Page 153 ANNEX 4 Acronyms sec4.qxd 7/12/05 9:52 AM Page 154 154 AAS AAT ACES ACS ADS AFM AGB AGN AGU AIV AKR ALICE ALMA AMIE AO APT APXS ASCA ASI ASIC ASPOC ATR AU AWG BeppoSAX BHE BLR CAA CBRF CCD CDS CDS CdTe CELIAS CEPHAG CERN CESR CETP CFHT CIR CIS CIVA CMB CME CMOS CNES CNR CNRS acronyms American Astronomical Society Anglo-Australian Telescope Atomic Clock Ensemble in Space Advanced Camera for Surveys (HST) Astrophysics Data System (NASA) Atomic Force Microscope Asymptotic Giant Branch Active Galactic Nuclei American Geophysical Union Assembly, Integration & Verification Auroral Kilometric Radiation Rosetta Orbiter UV imaging spectrometer Atacama Large Millimetre Array Asteroid Moon micro-Imager Experiment (SMART-1) Announcement of Opportunity Astronomers’ Proposal Tool Alpha-Proton-X-ray Spectrometer (Rosetta) Advanced Satellite for Cosmology and Astrophysics (Japan) Italian Space Agency Application Specific Integrated Circuit Active Spacecraft Potential Control (Cluster) Attenuated Total Reflection Astronomical Unit Astronomy Working Group (ESA) Satellite per Astronomia in raggi X (Italy/The Netherlands) banded hiss emission Broad Line Region Cluster Active Archive Cosmic Background Radiation Field Charge Coupled Device Coronal Diagnostics Spectrometer (SOHO) Centre de Données astronomiques de Strasbourg cadmium telluride Charge, Element and Isotope Analysis System (SOHO) Centre d’Etude des Phenomenes Aleatoires et Geophysiques (France) Centre Européen de Recherches Nucléaires (France) Centre d’Etude Spatial des Rayonnements (France) Centre d’Etudes des Environments Terrestres et Planetaires (France) Canadian-French-Hawaiian Telescope Corotating Interaction Region; Composite IR Spectrometer (Cassini) Cluster Ion Spectrometry Comet Infrared and Visible Analyser (Rosetta) Cosmic Microwave Background Coronal Mass Ejection Complementary Metal Oxide Semiconductor Centre National d’Etudes Spatiales Consiglio Nazionale della Ricercha (Italy) Centre National de la Recherche Scientifique (France) CNSA COBE Co-I CONSERT COPUOS COROT COS COSAC COSIMA COSPAR COSPIN COSTEP CP CPM CR CS CSA CSDS CsI CSIRO CTIO CTTS CV CVF CXB D-CIXS Chinese National Space Administration Cosmic Background Explorer (NASA) Co-Investigator Comet Nucleus Sounding Experiment by Radiowave Transmission (Rosetta) Committee for the Peaceful Use of Outer Space (United Nations) COnvection, ROtation and planetary Transits Cosmic Origins Spectrograph (HST) Comet Sampling and Composition Experiment (Rosetta) Cometary Secondary Ion Mass Analyser (Rosetta) Committee on Space Research Cosmic Ray & Solar Charged Particles Investigation (Ulysses) Comprehensive Measurements of the SupraThermal and Energetic Particles Populations (SOHO) Charge Parity Chemical Propulsion Module (BepiColombo) Carrington Rotation Control Centre Canadian Space Agency Cluster Science Data System caesium iodide Commonwealth Scientific & Industrial Research Organisation (Australia) Cerro Tololo Inter-American Observatory Classical T-Tauri Star Cataclysmic Variable Circular Variable Filter (ISOCAM) Cosmic X-ray Background DSRI DUO Demonstration of a Compact Imaging X-ray Spectrometer (SMART-1) Directorate of Human Spaceflight, Microgravity & Exploration (ESA) Directorate of Scientific Programmes (ESA) Digital Elevation Model Observatoire de Paris, Département Spatial Diffuse Interstellar Band Descent Imager/Spectral Radiometer (Huygens) Deutsches Zentrum für Luft- und Raumfahrt Data Processing Centre Data Processing Unit Disturbance Reduction System (LISA Pathfinder) Double Star Data System Deep Space Network Digital Signal Processor; Double Star Programme (China) Danish Space Research Institute Dark Universe Observatory (NASA) EAS ECF EC EDI EFW European Astronomical Society European Coordinating Facility European Commission Electron Drift Instrument (Cluster) Electric Field & Wave experiment (Cluster) D/HME D/SCI DEM DESPA DIB DISR DLR DPC DPU DRS DSDS DSN DSP sec4.qxd 7/12/05 9:52 AM Page 155 acronyms EGS EGSE EIRO EIT ELAIS ELF EM EP EPAC EPDP EPIC EPS EQM ERNE ESA ESAC ESLAB ESO ESOC ESRIN ESRO ESTEC EUSO EUV EW FEEP FES FET FGM FGS FGS-TF FIRST 155 European Geophysical Society Electrical Ground Support Equipment European Intergovernmental Research Organisation Extreme UV Imaging Telescope (SOHO) European Large Array ISO Survey Extremely Low Frequency Electrical Model, Engineering Model Equivalence Principle energetic particle instrument (Ulysses) Electric Propulsion Diagnostic Package (SMART-1) European Photon Imaging Camera (XMM-Newton) European Physical Society Electrical Qualification Model Energetic and Relativistic Nuclei and Electron experiment (SOHO) European Space Agency European Space Astronomy Centre (ESA) European Space Laboratory (former name of SSD/RSSD) European Southern Observatory European Space Operations Centre, Darmstadt (Germany) ESA’s Documentation and Information Centre (Italy) European Space Research Organisation European Space Research and Technology Centre, Noordwijk (The Netherlands) Extreme Universe Space Observatory Extreme Ultra-Violet equivalent width FOS FOV FP FPAG FPGA FSRQ FTE FTS FUSE FUV FWHM Field Emission Electric Propulsion Fine Error Sensor field effect transistor Flux Gate Magnetometer Fine Guidance Sensor (HST) Fine Guidance Sensor-Tunable Filter (JWST) Far Infrared and Submillimetre Space Telescope (now Herschel) Flight Model Finnish Meteorological Institute Faint Object Camera (HST) FOcal Reducer/low dispersion Spectrograph 2 (ESO VLT) Faint Object Spectrograph (HST) Field of View Fabry-Pérot Fundamental Physics Advisory Group (ESA) Field Programmable Gate Array Flat Spectrum Radio Quasar Flux Transfer Event Fourier Transform Spectrometer Far-UV Spectroscopic Explorer (NASA) Far-Ultraviolet Full Width at Half Maximum GaAs GC Gallium Arsenide Galactic Centre FM FMI FOC FORS2 GDASS GENIE GIADA GLIMPSE GMOS GMT GOLF GONG GOODS GR GRB GSE GSFC GSP GSTP GTO HASI HCS HCSS HEB HEIC HEMT HEW HFI HGA HIFI HIPS HPOC HR HRC HRSC HRTS HSC HST IAA IAC IAU IBIS ICC IDT IFE IFS ILEWG ILT ILWS IMEWG IMF IMPACT INT INMS Gaia Data Access & Analysis Study Ground-based European Nulling Interferometer Experiment Grain Impact Analyser and Dust Accumulator (Rosetta) Galactic Legacy IR Mid-Plane Survey Extraordinaire Gemini Multi-Object Spectrograph Greenwich Mean Time Global Oscillations at Low Frequency (SOHO) Global Oscillation Network Group Great Observatories Origins Deep Survey General Relativity Gamma Ray Burst Ground Support Equipment Goddard Space Flight Center (NASA) General Studies Programme (ESA) General Support & Technology Programme (ESA) Geostationary Transfer Orbit Huygens Atmospheric Structure Instrument Heliospheric Current Sheet Herschel Common Science System Hot Electron Bolometer Hubble ESA Information Centre High Electron Mobility Transistor Half Energy Width High Frequency Instrument (Planck) High-Gain Antenna Heterodyne Instrument for Far-IR (Herschel) Highly Integrated Payload Suite Huygens Probe Operations Centre Hertzsprung-Russell High-Resolution Channel (HST/ACS) High Resolution Stereo Camera (Mars Express) High-Resolution Telescope & Spectrograph Herschel Science Centre Hubble Space Telescope Instituto de Astrofísica de Andalucía Instituto de Astrofisica de Canarias International Astronomical Union Integral imager Instrument Control Centre Instrument Dedicated Team Instrument Front-End Integral Field Spectroscopy International Lunar Exploration Working Group Instrument-Level Test International Living With a Star programme International Mars Exploration Working Group Initial Mass Function; Interplanetary Magnetic Field In-situ Measurements of Particles And CME Transients (STEREO) Isaac Newton Telescope Ion & Neutral Mass Spectrometer (Cassini) sec4.qxd 7/12/05 9:52 AM Page 156 156 INTA IOA IPAC IR IRAM IRAS IRF-U ISAS ISDC ISGRI ISM ISO ISOC ISSI IST ISWT ITC ITT IUE IUPAP IWF acronyms Instituto Nacional de Técnica Aerospacial (Spain) Institute of Astronomy (Cambridge, UK) Infrared Processing Analysis Center Infrared Institut de Radioastronomie Millimétrique Infrared Astronomy Satellite Institute for Space Physics-Uppsala (Sweden) Institute of Space and Astronautical Science (Japan), now part of JAXA Integral Science Data Centre Integral Soft Gamma Ray Imager Interstellar Medium Infrared Space Observatory (ESA) Integral Science Operations Centre International Space Science Institute, Bern (Switzerland) Instrument Science Team Integral Science Working Team International Institute for Geo-Information Science and Earth Observation (NL) Invitation to Tender International Ultraviolet Explorer International Union of Pure and Applied Physics Space Research Institute Graz (A) JAXA JCMT JEM-X JIVE JPL JSOC JWG JWST Japan Aerospace & Exploration Agency James Clerk Maxwell Telescope Integral X-ray monitor Joint Institute for VLBI in Europe Jet Propulsion Laboratory (NASA) Joint Science Operation Centre (Cluster) Joint Working Group James Webb Space Telescope (formerly NGST) KATE X/Ka-band Telemetry & Telecommand Experiment (SMART-1) Kitt Peak National Observatory (USA) KPNO LAEFF LAP LASCO LBV LDAP LECS LET LETG LFI LIRG LISA LIST LMC LMXB LOI LP LPCE Laboratory for Space Astrophysics and Fundamental Physics Langmuir Probe (Rosetta) Large Angle Spectroscopic Coronagraph (SOHO) Luminous Blue Variable Lightweight Directory Access Protocol Low Energy Concentrator Spectrometer (BeppoSAX) Low Energy Telescope (Ulysses) Low-Energy Transmission Grating Low Frequency Instrument (Planck) Luminous IR Galaxy Laser Interferometer Space Antenna LISA International Science Team Large Magellanic Cloud Low Mass X-ray Binary Luminosity Oscillation Imager (SOHO) LISA Pathfinder Laboratoire de Physique et Chemie, de l’Environnement (France) LPF LPSP LPV LTE LTP LWS MAPPS MCP MDI MDPU MECS MER MHD Microscope MIDAS MIP MIRI MIRO MLH MLT MMO MOC MOLA MOS-CCD MoU MPAE MPE MPI MPIA MPIK MPO MRR MSE MSSL MUPUS MUSICOS MXB MXU NAC NASA NED NFI NGST NHSC NICMOS NIRSpec LISA Pathfinder Laboratoire de Physique Stellaire et Planétaire (France) Long-Period Variable Local Thermal Equilibrium LISA Technology Package Long Wavelength Spectrometer (ISO) Mapping & Planning for Payload Science (Venus Express) Microchannel Plate Michelson Doppler Imager (SOHO) Model Data Processing Unit Medium-Energy Concentrator Spectrometer (BeppoSAX) Mars Exploration Rover (NASA) Magnetohydrodynamics MICROSatellite à traînée Compensée pour l’Observaton du Principe d’Equivalence (CNES) Micro-Imaging Dust Analysing System (Rosetta) Mutual Impedance Probe (Rosetta) Mid-IR Instrument (JWST) Microwave Instrument for the Rosetta Orbiter (Rosetta) Mid-Latitude Hiss Magnetic Local Time Mercury Magnetospheric Orbiter (BepiColombo) Mission Operations Centre Mars Observer Laser Altimeter Metal Oxide Semiconductor Charge Coupled Device Memorandum of Understanding Max-Planck-Institut für Aeronomie Max-Planck-Institut für Extraterrestrische Physik Max-Planck Institut (Germany) Max-Planck-Institut für Astronomie Max-Planck-Institut für Kernphysik Mercury Planetary Orbiter (BepiColombo) Mission Risk Review Mercury Surface Element (BepiColombo) Mullard Space Science Laboratory (UK) Multi-Purpose Sensors for Surface and Subsurface Science (Rosetta) Multi-Site Continuous Spectroscopy Medium X-ray Band Mask Exchange Unit Narrow Angle Camera (OSIRIS) National Aeronautics & Space Administration (USA) NASA Extragalactic Database Narrow Field Instrument (BeppoSAX) Next Generation Space Telescope (now James Webb Space Telescope) NASA Herschel Science Center Near-Infrared Camera and Multi-Object Spectrometer (HST) Near-IR Spectrometer (JWST) sec4.qxd 7/12/05 9:52 AM Page 157 acronyms NIS NLR NOAO 157 normal incidence spectrometer Narrow Line Region National Optical Astronomy Observatories (US) Nordic Optical Telescope National Radio Astronomy Observatory (USA) National Space Science Data Center (at GSFC, USA) National Synchotron Light Source (USA) New Technology Telescope NRAO/VLA Sky Survey RMOC ROLIS ROMAP Osservatorio Astronomico di Trieste Observatoire de Haute-Provence Optical Monitor (XMM-Newton) Optical Monitor Camera (Integral) Optical and Spectroscopic Remote Imaging System (Rosetta) RTG SAS PWG Photodetector Array Camera and Spectrometer (Herschel) Polycyclic Aromatic Hydrocarbon parsec Photon Counting Detector Payload Definition Document Particle Detector Front End Phoswich Detector System Principal Investigator (ISO)PHOT Interactive Analysis Planetary Ion Camera (BepiColombo MPO) Passivated Implanted Planar Silicon Payload Module Pre-Main Sequence Planetary Nebula (plural: PNe) Payload Operations Service (Mars Express) Permittivity Probe (SESAME on Rosetta) parts per million Public Relations Project Scientist Planetary Science Archive Project Scientist Team; Payload Support Team Point Spread Function Planck Science Office Permitivity, Waves and Altimetry (part of HASI on Huygens) Payload Working Group QED QM QPD QPO QSO Quantum Electrodynamics Qualification Model Quadrant Photodiode Quasi Periodic Oscillation Quasi Stellar Object R&D RAID RAL RF RGS Research and Development Redundant Array of Inexpensive Disks Rutherford Appleton Laboratory (UK) Radio Frequency Reflection Grating Spectrometer (XMMNewton) Reuven Ramaty High Energy Solar Spectroscopic Imager (NASA) NOT NRAO NSSDC NSLS NTT NVSS OAT OHP OM OMC OSIRIS PACS PAH pc PCD PDD PDFE PDS PI PIA PICAM PIPS PLM PMS PN POS PP ppm PR PS PSA PST PSF PSO PWA RHESSI ROSINA ROSITA RPC RSI RSOC RSSD SAFIR SAO SAp/Saclay SAX SBC SCAM SciSIM SCOS SCR SDT SED SEM SEP SEPM SEPP SEPT SESAME SEST SETI SFH SFR SIMBA SIMBAD SIR SIRTF SIS SLP SM SMART SMC SMEX SMOG SN Rosetta Mission Operations Centre Rosetta Lander Imaging System RoLand Magnetometer & Plasma Monitor (Rosetta) Rosetta Orbiter Spectrometer for Ion and Neutral Analysis (Rosetta) Roentgen Survey with an Imaging Telescope Array Rosetta Plasma Consortium Radio Science Investigation Rosetta Science Operations Centre Research and Scientific Support Department (ESA) Radioisotope Thermoelectric Generator Single Aperture Far-IR (NASA) Smithsonian Astrophysical Observatory (USA) Service d’Astrophysique (Commissariat à l’Energie Atomique; Saclay, France) Scientific Analysis Software (XMMNewton); Science Analysis Subsystem (XMM-Newton) Satellite per Astronomia in raggi X (Italy/The Netherlands) Solar-Blind Channel (ACS/HST) Superconducting Camera Science Simulator Spacecraft Operations System Software Change Request Science Definition Team Spectral Energy Distribution Scanning Electron Microscope solar energetic particle; solar electric propulsion; solar electron proton Solar Electric Propulsion Module (BepiColombo) Solar Electric Primary Propulsion Solar Energetic Particle Telescope (STEREO) Surface Electric, Seismic and Acoustic Monitoring Experiment (Rosetta) ESO sub-mm telescope Search for Extra-Terrestrial Intelligence Star Formation History Star Formation Rate SEST Imaging Bolometer Array Set of Identifications, Measurements and Bibliography on Astronomical Data Stream Interacting Region Space Infrared Telescope Facility (NASA; now Spitzer) Superconductor-Insulator-Superconductor Segmented Langmuir Probe Servicing Mission (Hubble) Small Mission for Advanced Research in Technology (ESA) Small Magellanic Cloud Small Explorer (NASA) Survey of Molecular Oxygen in the Galaxy (SMART-1) Supernova sec4.qxd 7/12/05 9:52 AM Page 158 158 SNR SOC SOHO SOI SOS SOT SOWG SPC SPECS SPEDE SPI SPICAM SPIRE SPR SQUID SRON SRR SRV SSAC SSC SSD SSP SSWG ST ST-ECF STAFF STEREO STIS STJ STOC STScI SUMER SWAN SWAS SWS SWT SVM SXB SXT SZ TAC TNG ToO TPF TRACE TRIP acronyms Supernova Remnant Science Operations Centre; self-organising criticality Solar and Heliospheric Observatory Saturn Orbit Insertion Silicon-on-Sapphire Science Operations Team Science Operations Working Group Science Programme Committee (ESA) Submillimeter Probe of the Evolution of Cosmic Structure (NASA) Spacecraft Potential, Electron & Dust Experiment (SMART-1) Integral spectrometer Mars Express UV Spectrometer Spectral and Photometric Imaging Receiver (Herschel) Software Problem Report Superconducting Quantum Interference Device Space Research Organisation Netherlands System Requirement Review Semi-Regular Variable Space Science Advisory Committee (ESA) Survey Science Consortium (XMM-Newton) Space Science Department (ESA), now RSSD Surface Science Package (Huygens and Rosetta) Solar System Working Group (ESA) Science Team; Space Technology (NASA) Space Telescope European Coordinating Facility (Germany) Spatio-Temporal Analyis of Field Fluctuations (Cluster) Solar-Terrestrial Relations Observatory (NASA) Space Telescope Imaging Spectrograph Superconducting Tunnel Junction Science & Technology Operations Coordination Space Telescope Science Institute Solar UV Measurements of Emitted Radiation (SOHO) Solar Wind Anisotropies (SOHO) Submillimeter Wave Astronomy Satellite (NASA) Short Wavelength Spectrometer (ISO) Science Working Team Service Module Soft X-ray Band Soft X-ray Telescope (Yohkoh) Sunyaev-Zeldovich Effect Time Allocation Committee Telescopio Nazionale Galileo Target of Opportunity Terrestrial Planet Finder (NASA) Transition Region & Coronal Explorer (NASA) Technology Readiness and Implementation Plan TRL TRM TRP TRS TSI Technology Readiness Level Technology Reference Mission Technology Research Programme (ESA) Technology Reference Study Total Solar Irradiance UCB UCLA ULIRG URSI USNO UT UV UVCS UVES University of California Berkeley (USA) University of California Los Angeles (USA) Ultra-Luminous IR Galaxy Union Radio Scientifique Internationale US Naval Observatory Universal Time Ultraviolet Ultra-Violet Coronal Spectrometer (SOHO) Ultraviolet-Visual Echelle Spectrograph (ESO VLT) UV Imaging Spectrometer (Cassini) UVIS VILSPA VIMOS VIMS VIRGO VIRTIS VLA VLBI VLF VLT VLTI VO VSOC VTT WAC WBD WEC WFC WFPC WHISPER WHT WIYN WMAP WWW XEUS Villafranca Satellite Tracking Station VLT Visible Multi-Object Spectrograph (ESO VLT) Visual IR Mapping Spectrometer (Cassini) Variability of Irradiance and Gravity Oscillations (SOHO) Visible Infra Red Thermal Imaging Spectrometer (Rosetta) Very Large Array Very Long Baseline Interferometry Very Low Frequency Very Large Telescope Very Large Telescope Interferometer (ESO VLT) Virtual Observatory Venus Express Science Operations Centre Vacuum Tower Telescope Wide Angle Camera (OSIRIS on Rosetta) Wide Band Data (Cluster) Wave Experiment Consortium (Cluster) Wide-Field Camera (HST) Wide-Field Planetary Camera (HST) Waves of High Frequency and Sounder for Probing of Density by Relaxation (Cluster) William Herschel Telescope Wisconsin Indiana Yale NOAO (US) Wilkinson Microwave Anisotropy Probe (NASA) World Wide Web XSA X-ray Evolving Universe Spectroscopy mission (ESA) X-ray Multi-Mirror Mission (ESA); now XMM-Newton XMM-Newton Science Archive (ESA) YGT YSO Young Graduate Trainee Young Stellar Object ZAMS Zero Age Main Sequence XMM
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