Click Here JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, A07S30, doi:10.1029/2007JA012770, 2008 for Full Article Multispacecraft observation of electron beam in reconnection region A. Åsnes,1 M. G. G. T. Taylor,1 A. L. Borg,2 B. Lavraud,3 R. W. H. Friedel,3 C. P. Escoubet,1 H. Laakso,1 P. Daly,4 and A. N. Fazakerley5 Received 27 August 2007; revised 29 November 2007; accepted 8 January 2008; published 10 May 2008. [1] On the 18th of August 2002, during a crossing of the near-Earth plasma sheet Cluster observed an ion flow burst, caused by a near-Earth reconnection event. Cluster observed a tailward bulk flow which reverse to earthward flow, indicating a close passage of the diffusion region. We show that reversals in BZ and BY are consistent with reconnection. During the event, a short duration burst of electrons in the range of a few keV up to more than 100 keV are observed streaming away from the reconnection region. The accelerated electrons were aligned with the magnetic field, streaming tailward, and were observed simultaneously by all four spacecraft located on both the northern and southern side of the current sheet. The four Cluster spacecraft, separated by 3700 km, observe the electrons for a time period of 60 s, indicating the burst to be a temporal rather than localized feature. A second burst of tailward accelerated electrons observed for 40 s was observed by Cluster 1 and 2 upon entering the earthward outflow region. The second beam thus appear to be directed toward the X-line. The flux levels of the energetic electron bursts exceed those of the ambient plasma sheet by a factor 2–4. In general, the highest energetic electron fluxes during this event were observed in the earthward outflow region. Observations indicate that reconnection operates on closed plasma sheet field lines in this event and does not reach lobe field lines. Citation: Åsnes, A., M. G. G. T. Taylor, A. L. Borg, B. Lavraud, R. W. H. Friedel, C. P. Escoubet, H. Laakso, P. Daly, and A. N. Fazakerley (2008), Multispacecraft observation of electron beam in reconnection region, J. Geophys. Res., 113, A07S30, doi:10.1029/2007JA012770. 1. Introduction [2] Bursts of energetic particles in the Earth’s magnetotail have been reported since early satellite observations [Sarris et al., 1976] and have often been associated with reconnection. Magnetic reconnection generally takes place in current sheets separating field lines of opposite directionality, leading to a change of the field line topology [Vasyliunas, 1975]. In this process magnetic energy is converted into kinetic energy of the plasma, which can be manifested in various ways. For reconnection to be allowed, the particles must be decoupled from the magnetic field, within a diffusion region. Owing to the larger mass and gyroradius, ions will have a larger diffusion region compared to electrons. This leads to differential motion of ions and electrons which give rise to the Hall current system [Sonnerup, 1979; Nagai et al., 2001]. Plasma jets of ion outflow from the X-line in the current sheet (CS) plane 1 ESA/ESTEC, Nordwijk, Netherlands. Norwegian Defence Research Establishment, Kjeller, Norway. Space Science and Applications, Los Alamos National Laboratory, Los Alamos, New Mexico, USA. 4 Max Planck Institute for Solar System Research, Katlenburg-Lindau, Germany. 5 Mullard Space Science Laboratory, Dorking, UK. 2 3 have a velocity related to the inflow velocity of the plasma into the X-line [Sonnerup et al., 1981]. Relatively strong induced electric fields, in the dawn-dusk direction, in the region surrounding the X-line are able to accelerate demagnetized particles during their meandering/Speiser motion [Sato et al., 1982; Hoshino et al., 2001]. In addition, a secondary acceleration in the magnetic field pile up region of the reconnection outflow have been proposed [Hoshino et al., 2001]. Particle in cell (PIC) simulations show that electrons will gain energy in this region due to gradient and nonadiabatic curvature drift antiparallel to the induced electric field. Drake et al. [2005] presents an alternative acceleration mechanism based on PIC simulations, where electrons are trapped and accelerated by a Fermi mechanism within collapsing miniature islands of magnetic flux. Observations of such a miniature island in a near-Earth reconnection event was recently described by Eastwood et al. [2007]. Another possible mechanism related to reconnection is stochastic acceleration through turbulence or wave-particle interaction [Ambrosiano et al., 1988; Shinohara et al., 1998]. [3] While ions gain most of their energy with their bulk outflow velocity, a flow velocity of 1000 km/s will increase electron energy by only a few eV. However, electrons might gain thermal energy more efficiently in the diffusion region due to their low mass compared to the heavier ions. Copyright 2008 by the American Geophysical Union. 0148-0227/08/2007JA012770$09.00 A07S30 1 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 1. Positions of the Cluster spacecraft relative to Cluster 3 (17.7, 5.0, 3.4) RE GSM. Relative position (a, b) in GSM-coordinates and (c, d) in current sheet coordinates. See text for details. [4] Previous observations have shown that on the reconnection separatrices (separating reconnected from the prereconnected field lines) low-energy electrons are streaming into the X-line while high-energy electrons accelerated in the reconnection region are streaming away from the X-line [Nagai et al., 2001; Manapat et al., 2006]. The low-energy electrons are carrying the reconnection Hall current, while the energetic part is accelerated electrons escaping along the field. Detailed observations of low-energy electrons streaming into a near-Earth X-line on the plasma sheet boundary layer have been shown by Asano et al. [2006] using four spacecraft Cluster data. A strong beam of energetic electrons within the plasma sheet has also been reported Taylor et al. [2006], which might be reconnection-related. [5] This study is based on a list of 13 reconnection events previously identified in the Cluster data [Borg, 2006], where we have examined the energetic electron observations to look for signatures of accelerated electron beams similar to the event of Taylor et al. [2006]. Of the 13 events, none had a beam of the intensity reported by Taylor et al. [2006]. However, all events where high-resolution electron data were available did show evidence of unidirectional streaming energetic (suprathermal) electrons, which we will term beams in this paper. These beams area identified as a flux increase in the electrons along the magnetic field, directed away from the reconnection region. We present one event here, where all four spacecraft simultaneously observe an electron beam. Of primary interest is that during this event Cluster 3 is positioned on the opposite side of the current sheet. We believe this to be the first report where highenergy electron beams are observed on opposite sides of the current sheet simultaneously. 2. Instrumentation [6] The Cluster spacecraft have a spin period of 4 s, such that the particle detectors and plasma instruments (RAPID, PEACE, and CIS) [Wilken et al., 2001; Johnstone et al., 1997; Rème et al., 2001] will sample the entire 4p sphere in 4 s. As we are interested particularly in the look directions aligned with the magnetic field we note that each of these two directions, parallel and antiparallel, is generally sampled once per spin, and with half a spin period (2 s) in between measurements in the two directions if the magnetic field direction remains constant. In this event we have burst mode (BM) data available, which provides us with good resolution in both energy and look directions. For this event we use full three-dimensional data from the PEACE HighEnergy Electron Analyzer (HEEA) sensor which was operating with a spatial resolution of 30° (polar angle), 11.25° (azimuthal angle). In the case of RAPID IES (Imaging Electron Spectrometer) has a resolution of up to 20° 22.5°. FGM magnetic field data [Balogh et al., 2001] are presented with a resolution of five vectors per second. Ion flow velocities are from the CIS instrument, using the Hot Ion Analyzer on spacecraft 1 and 3, while Composition 2 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS Figure 2. Overview of magnetic field and plasma bulk flow. The data are presented in current sheet coordinates, with Z 0 along the current sheet normal and X 0 XGSM direction (see text for details). First, second, and third panels show FGM data in directions of maximum, medium, and minimum variation, respectively. Fourth and fifth panels show CIS ion plasma flow in the X 0 direction and the total flow perpendicular to the magnetic field, respectively. The intervals of electron beams is indicated by boxes above the first panel, color coded for time of observation at individual spacecraft. Distribution Function (CODIF) analyzer is used on spacecraft 4. 3. Cluster Observations [7] We consider Cluster observations in the interval 1700 – 1720 UT on 18 August 2002 during which time magnetospheric conditions were relatively quiet, with no evidence of significant substorm or geomagnetic activity. The solar wind conditions were calm at this time, with an interval of weak southward interplanetary magnetic field (IMF) BZ preceding the event. The Cluster spacecraft were located at GSM X, Y, Z = [17.7, 5.0, 3.1] RE in the downtail plasma sheet with an average separation of 3700 km (Figure 1). A07S30 [8] Figure 2 shows an overview of the magnetic field and ion flows (VX 0) and V? during the event. The data is presented here in a current sheet coordinate system, where Z 0 is the estimated current sheet normal, X 0 is in the direction of maximum variation (XGSM) and Y 0 completes a right-hand system. To obtain the orientation of the current sheet plane, we use minimum variance analysis (MVA) [Sonnerup and Cahill, 1967; Haaland et al., 2006] applied to the FGM data of an interval just prior to the first tailward flow burst, from 1658 to 1702 UT, while C1, C2, and C4 is crossing the current sheet from south to north. We apply the MVA-algorithm to the four spacecraft magnetic field data ensemble, to obtain an average current sheet orientation. The eigenvalues and vectors represented in GSM coordinates are given in Table 1. The coordinate transform is necessary in this event, in order to see the reconnection signatures, Hall BY and reversal of BZ, clearly, and we will present data in the X 0, Y 0, Z 0 coordinate system throughout this paper. We note that MVA-analysis applied to current sheet crossings by C1 and C4 at 1707:40 – 1707:40 UT, which would seem like a natural choice for this analysis, appear to be significantly influenced by Hall-currents. [9] At the beginning of the period, considering the X 0component of the magnetic field, C1 and C4 are north of the current sheet (CS). C2 is located closer to but mainly north of the CS and C3 is below the CS. Around 1703 UT a tailward plasma flow is observed together with southward BZ 0, interpreted to be caused by reconnection Earthward of Cluster. At around 1707:30 UT C1 and C4 move south of the NS and shortly after, 1708:30 UT, detect a flow and BZ 0 reversal, suggesting that the X-line moves tailward of Cluster. At C3 the tailward bulk flow cease around 1708 UT, accompanied by a decrease in temperature and density (not shown) but still remains in the plasma sheet. This indicates that C3 either moved to the reconnection inflow region or alternatively that the reconnection is rather localized or filamentary in this case. We note that ion data is not available from C2, but PEACE moment calculations of electron bulk flow (not shown) indicate a lack of flow reversal also at C2. After 1709:30 UT C1 and C4 observes another brief interval of weak tailward plasma flow before the flow turns earthward again until 1715 UT. [10] We illustrate the BY 0 variations observed by C4 as function of VX 0 and BX 0 in Figure 3. The signs of VX 0 and BX 0 determine which quadrant of the Hall-current system is observed, as illustrated in the top left inset. The core BY 0 field of 4.7 nT was estimated by the average BY 0 field prior to the event. The BY 0 variations at C4 can be seen to match well with predicted Hall effects, and this is also the case for C1. At C3 the BY 0 deflections are not consistent with Hall effects and also at C2 the initial positive BY 0 perturbations does not appear consistent with Hall effects considering that Table 1. Results of Minimum Variance Analysis of 4SC Magnetic Field Data From 1658 to 1702 UT a Eigenvalue Maximum (X 0) Medium (Y 0) Minimum (Z 0) 3 of 11 a 62.4 0.925 0.045 Eigenvector (X, Y, Z GSM) 0.939 0.340 0.049 Eigenvectors are expressed in GSM coordinates. 0.323 0.823 0.467 0.119 0.454 0.883 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 3. Cluster 4, BX0 versus VX0 with BY0 represented as circles for the 1704– 1714 UT interval. Circle size indicate dBY0 = BY0 4.7 nT, where 4.7 nT is the estimated core BY0 field. The inset figure in the top left quadrant illustrate the reconnection geometry with Hall fields. the flow here is almost certainly tailward from 1703 to 1707:30 UT. This indicates that C3 and initially also C2 is located in a region away from the Hall currents. [11] In Figure 4 we focus on the time interval of the beam observation at all 4 Cluster spacecraft, using RAPID pitch angle distributions from the lower-energy channel (41.7 – 52.7 keV). We note that although the signal is very close to the background noise level, there are clearly distinguishable beam signatures at all four spacecraft. The magnetic field and ion flow signatures are consistent with the four spacecraft being located tailward of the reconnection X-line, with C1, C2, and C4 on the north side, and C3 on the south side of the current sheet. From 1705:45 to 1706:05 UT C1 and C4 observe enhanced fluxes in the antiparallel direction. A similar signature is seen at C2 over a longer period (1705:20 – 1706:20 UT) with a more isotropic appearance coinciding with the proximity of C2 to the current sheet. At C3 the enhancement of flux (1705:15 – 1705:25 UT) is in the opposite direction, parallel to the magnetic field, but due to C3 position below the current sheet it is consistent with tailward directed fluxes at all four spacecraft. Owing to the alignment of these enhancements with the magnetic field we will refer to them as beams and a more detailed view of these beams is presented in Figure 6 where we show data from Cluster 1 only. [12] We use observations from Cluster 4 in Figure 5 to provide an overview of the electron behavior during this event. The observations at C1 are generally very similar to those at C4, while C2 and C3 show differences resulting from different location relative to the X-line geometry. The top panel in Figure 5 shows spin averaged electron fluxes from RAPID, for five energy channels (41.7 – 237.5 keV). The second panel shows the PEACE energy-time spectrogram of energy flux. The third and fourth panels show PEACE energy-time spectrograms of anisotropy and j? jk , and streaming. Anisotropy is defined here as j? þ jk jka jkb streaming as where j is the measured flux and ka jka þ jkb and kb denote the parallel and antiparallel along the magnetic field direction B, respectively. The time of the electron beam at C4 (1705:52– 1706:05 UT) is marked with an arrow in the RAPID data panel. The spacecraft is initially located in the plasma sheet, characterized by several KeV electron energies, but moves out into a colder and less dense plasma in the middle of the interval. The third panel shows the plasma during this interval to be mostly bidirectional (blue color) at most energies. At the start of the plasma bulk flow interval (1703 UT) the distribution is becoming more strongly field aligned (deep blue) at energies up to a few keV. The fourth panel shows a measure of the streaming of the plasma sheet electrons; the balance of fluxes in the field aligned and anti-field-aligned directions. Before and after the event, the fluxes are well balanced in the two directions, shown as black. Once the tailward flow initiates, one can see that antiparallel electrons dominate (blue) as long as the spacecraft is north of the current sheet (interval A – B). When C4 moves south of the current sheet (marked with vertical line B) this streaming turns field aligned (yellow) for 30 s until C4 is moving into a colder, less dense electron plasma. This electron streaming is not an observation of the plasma flow as the ion bulk flow velocity is negligible compared to the electron thermal velocities. [13] The beam (1705:52– 1706:05 UT) does not display the most intense fluxes during the period. The electron fluxes at the time of the current sheet crossing (1707:30, line B) are comparable to the beam, while the most intense fluxes observed by RAPID coincide with intervals of 4 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 4. Electron beam observed by RAPID on all four spacecraft. Panels show pitch angle distribution versus time from Cluster 1, 2, 3, and 4, at energy 41.7 – 52.7 keV. earthward directed plasma flow (the intervals marked C– D and E– F in Figure 5). An asymmetry between energetic electron fluxes in the earthward and tailward outflow regions have been discussed previously by Imada et al. [2005, 2007] and can be interpreted as evidence for a twostep acceleration [Hoshino et al., 2001; Hoshino and Mukai, 2002]. The reason for the Earthward/tailward asymmetry would be due to the intrinsic dipole field of the Earth which lead to a stronger magnetic field pile-up effect on the earthward side. The lack of an electron flux maxima observed by C1 and C4 in the flow reversal region is contrary to observations made by Wind in a diffusion region at X = 60 RE discussed by Øieroset et al. [2002]. This discrepancy is most likely due to Cluster not going through the diffusion region itself but passing it on the southern side from the tailward to earthward outflow region. This view is supported from Figure 3, where BX 0 = 15 nT during the time of flow reversals, whereas it should approach zero near the X-line. In the plasma flow we do not observe expected signatures of being in the plasma inflow direction, a stagnation in the VX component accompanied by an inflow of plasma (VZ). However, C1 and C4 observe a 15 s interval of constant 100 km/s flow prior to the first earthward flow (time C), which is of the same order as the deduced tailward motion of the X-line, calculated from the reversal signature in C1 and C4. From the PEACE spectrogram in the second panel we notice that the electron population is relatively cool and tenuous around the time of flow reversals, possibly corresponding to a preaccelerated plasma in the inflow region. [14] From the perpendicular flow components in X 0 and 0 Y directions, shown as red traces in Figure 5, the fifth and sixth panels, we note that the magnetic flux-carrying flow is mostly in the Y 0 direction, except when C4 is crossing the current sheet. Also, the perpendicular component is small during the earthward flow intervals (C– D and E– F). [15] In Figure 6 we show the full resolution electron data for selected energy channels from RAPID (first and second panels) and PEACE (third through fifth panels) together with ion plasma flow in X 0 and Y 0 directions. The bottom panel shows the X 0, Y 0 and Z 0 magnetic field components. The electron panels show data by polar sectors versus time, at subspin resolution. Contours of pitch angles sampled in the look directions are superposed, with solid black, dashed black, and solid white lines indicating parallel, 90° and antiparallel pitch angles, respectively. The offset between pitch angle contours of RAPID and PEACE results from the 5 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 5. Overview of C4 electron population in reconnection interval. Top panel gives RAPID flux for five energy channels (41.7 –237.5 keV). Second through fourth panels are from PEACE and show energy time, anisotropy, and streaming spectrograms respectively (see text for details). Fifth and sixth panels show the CIS plasma flow in X 0 and Y 0 directions, with perpendicular (to B) components in red. Seventh panel shows X 0 (red), Y 0 (blue), and Z 0 (green) components of magnetic field. locations the instruments are mounted on the spacecraft. RAPID is mounted 90° in the direction of the rotation from PEACE HEEA such that RAPID will look in the (anti-)field-aligned direction 1/4 of a spin (1 s) prior to PEACE HEEA. [16] Starting from high-energy, RAPID (41.7 –70.3 keV) shows that from one spin to the next, significant flux suddenly is seen in the anti-field-aligned direction (inside white contours). This enhancement is most intense initially and lasts for only three spin periods. At PEACE we note that the enhancement in the two upper channels (8.6– 12.2 and 3.6– 5.5 keV) last only two spins, where between the antiparallel observation at RAPID (1706:01 – 1706:02 UT) and the PEACE moving into that look direction, the beam 6 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 6. Electron beam in RAPID and PEACE on Cluster 1. Polar ranges plotted against time at subspin time resolution. Pitch angle contours are overlain; field-aligned (30° and 60°): black, perpendicular (90°): dashed black, anti-field-aligned (120° and 150°): solid white. Bottom three panels give FGM BX, BY and BZ components. flux had significantly decreased. In the 0.9 – 1.5 keV PEACE channel the main change during the beam is a flux increase in the perpendicular direction, although the distribution remain field aligned. [17] We are not able to discern any dispersion effects here, as the beam appears simultaneously at all energies, within the energy range of the two instruments. In the lower-energy range (<1 keV) of PEACE, the fluxes are bidirectional even before the beam occurs, and there appear to be no significant change in this energy range. [18] Concurrent with the electron beam there is also a signature in the magnetic field, shown in the bottom three panels of Figure 6. During a 6 s interval, corresponding well to the beam interval as seen in PEACE, BY 0 is reduced by more than 3 nT, while BZ 0 shows a negative deflection before and possibly also after the negative BY 0 deflection. This magnetic signature observed both by C1 and C4 indicates that there is a significant current related to the event. We have not been able to estimate the current configuration or intensity, as only two spacecraft observe 7 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 7. Second electron beam event, observed only at C1 and C2. First though third panels show C1 PEACE and RAPID data, while fourth through sixth panels show C2 data. First and fourth panels show PEACE energy spectrum. Second and fifth panels show RAPID pitch angle data. Third and sixth panels are streaming spectrogram as in Figure 5. Seventh and eighth panels show the BX0 and BZ0 component for C1 (black) and C2 (red). Bottom panel shows the C1 VX0 component of ion plasma flow. it, and also the magnetic signature cannot be interpreted as being caused by a 1-D current sheet. At C3 the electron beam is observed without a similar magnetic signature, while at C2 the magnetic field variations are more complex. [19] A second electron beam was observed by C2 and C1 in the time interval 1708:27 – 1708:58 UT, presented in Figure 7. At 1708:27 – 1708:40 UT C2 observes the beam, in the field-aligned (tailward) direction. Directly after the 8 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS A07S30 Figure 8. Electron spectra from PEACE and RAPID during the beams, ordered by start time. Spectra are ordered by pitch angle, with 0 – 30° in red, 70– 110° in black, and 150– 180° PA in blue. flow reversal from tailward to earthward, C1 also observe a field-aligned electron beam (tailward) lasting for 20 s, before the flux intensifies in all directions. As C1 is observing both a BZ 0 and flow reversal prior to the beam observation, it is located earthward of an X-line during the beam. This implies that the high-energy electron beam is directed toward the X-line, contrary to the first beam where all observations showed the beam directed away from the X-line. At C2 we do not have the ion flow information, but the reversal in BZ 0 occurs during the beam. The electron plasma at C2 does not show an increase in temperature and density similar to what is seen by C1 during the earthward flow, indicating that C2 does in fact not enter the earthward flow at this time. C4 enters the earthward flow only 20 s after C1 but does not observe a similar beam. [20] The electron spectra measured during the beams, observed by PEACE and RAPID, are shown in Figure 8, ordered by their time of observation. In the first beam, shown in Figures 8a to 8d, the difference between parallel and antiparallel fluxes is only apparent starting from a few keV, above the peak energy of the distribution. In the lowerenergy part, the flux is balanced between the two direction. It should be noted that the most intense beam in the RAPID energy range is seen by C3. C3 is also isotropic in the PEACE range around the peak energy, unlike the other spacecraft where the distribution is field aligned at peak energy. In the second beam, in Figures 8e and 8f, the beam is observed in a lower density, cooler plasma. However, the flux intensity in the RAPID energy range is nearly the same as seen in the first beam (at C1, C2, and C4). It should also 9 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS be pointed out that from the six beam observations presented here, all of them are directed tailward, with an increase in the parallel (antiparallel) direction south (north) of the current sheet. 4. Discussion and Summary [21] We have described a reconnection event from the point of view of energetic and accelerated electrons. The reconnection event was identified from ion plasma flow reversal, with corresponding BZ reversal and Hall magnetic field signatures. The first electron beam event is unique as the beam is not only observed by four spacecraft but also with C3 on the opposite side of the current sheet compared to the other spacecraft. [22] The four Cluster spacecraft are initially tailward of the X-line, the existence of which is first indicated at 1703 UT when a tailward plasma flow is observed. At this time C1, C2, and C4 are north of the current sheet, and C3 is on the south side. Around 1707 UT, after the first beam, C2 followed by C1 and C4 moves south of the current sheet. After 1708 UT C1 and C4 enters into the earthward outflow region, while C3, due to the absence of flow at this time, is presumably outside of this region but still within the plasma sheet observing a colder, less dense plasma. [23] We highlight the following characteristics of these observations: (1) a persistent outflow away from the X-line of field-aligned electrons at energies higher than the nominal plasma sheet energy (>2 keV) observed by PEACE, (2) a short-lived (1705:15 – 1706:10 UT) accelerated electron beam, directed away from a X-line earthward of the tetrahedron, observed by all four spacecraft. (3) An additional beam feature observed only at C1 and C2, interpreted to be in the direction towards the X-line at C1, right after C1 moves into the earthward flow region (1708:30– 1709:00 UT). (4) An absence of low-energy electrons counterstreaming against the high-energy beam. (5) No peak of accelerated electrons associated with the time of flow reversal. Therefore, we suggest that the diffusion region is not directly sampled. (6) High fluxes of energetic electrons coincide with earthward flow intervals. [24] The continuous weak streaming of the electrons above 2 keV away from the reconnection region may be interpreted as ongoing acceleration in a wide region around the X-line. Following the acceleration, electrons subsequently escape along the field line to reach the spacecraft. As the spacecraft is presumably on closed field lines based on the observed trapped population, this implies that some part of the electrons must be lost before being either magnetically mirrored or have bounced all the way around the closed field line structure (plasmoid). The observation is consistent with acceleration in a magnetic field pile up region surrounding the diffusion region [Hoshino et al., 2001]. [25] The electron beam at 1705 – 1706 UT, observed by all four spacecraft, may be interpreted to originate in the X-line itself, which means that it should be observed close to the reconnection separatrix. In order for the beam to be seen more or less at the same time at all spacecraft separated by thousands of kilometers, this would imply a rapid burst of reconnection. Subsequently, the separatrix A07S30 would expand rapidly and move over each spacecraft. However, Cluster does not show other clear indications of crossing a separatrix at this time. In particular we note an absence of low-energy electrons streaming into the X-line during these beams, contrary to what is commonly observed [Nagai et al., 2001]. [26] Another possible interpretation is that the beam is caused by a temporary intensification of the ongoing acceleration taking place in a wider region around the X-line, e.g., by rapid intensification of inductive electric fields. For either of these explanations, it seems that the reconnection process is bursty at this time and cannot be considered to be a steady state process. Overall, the reconnection event is interpreted to last for the duration of the flow burst (1703 – 1715 UT). [27] The second beam observed only by C1 and C2 does not easily fit in the current reconnection picture, as the beam at C1 is directed toward the X-line. The beam extends to such high energies (>70 keV) that it can not easily be explained by a field-aligned potential, a mechanism which is generally invoked for the low-energy electrons streaming toward the X-line. It is possible that the beam at C1 has been magnetically mirrored at low altitudes, only to return in the opposite direction of the initial acceleration. Another possibility is that there are more than one X-line, with the electron beam originating from a X-line on the earthward side. The case of more than one X-line would also allow for acceleration in contracting magnetic islands as suggested by Drake et al. [2006]. [28] Although we do observe reconnection accelerated electrons in this event, the observed intensity is far from overwhelming. The energetic electron flux in the beams exceeds the previous plasma sheet fluxes by a factor 2 – 3. The overall highest fluxes in the event occur in the earthward outflow region, where the energetic electron fluxes are isotropic. Our observations generally resembles the simulation results of Hoshino et al. [2001, Plate 3]. [29] The geomagnetic activity during this event is not significant, and the near-Earth reconnection event does not appear to occur with a substorm. The observation that C3 (and probably C2) is exiting the reconnection outflow region, while remaining on closed field lines, indicate that the reconnection X-line does not reach the lobe field lines in this event. Reconnection of lobe field lines is expected to proceed much faster and release more energy than reconnection of plasma sheet field lines, which may explain why there is no substorm related to this event [Baker et al., 1996]. The degree of particle acceleration may also be different in a plasma sheet reconnection event compared to the more rapid lobe reconnection events. [30] Finally, we note that after the reconnection event there has been no significant increase in plasma sheet temperature or energetic electron fluxes compared to the initial state. This indicates that an isolated reconnection event such as described here only provides very localized acceleration and that a substorm is required to heat the entire plasma sheet, such as is commonly seen. [31] Acknowledgments. Most plots in this paper were produced using the PaPCo software package. We thank H. Rème and E. Lucek for providing CIS and FGM data, respectively, through the CAA. A. Åsnes is grateful for helpful discussions with S. E. Haaland and M. Dunlop. 10 of 11 A07S30 ÅSNES ET AL.: RECONNECTION RELATED ELECTRON BEAMS [32] Wolfgang Baumjohann thanks Marit Øieroset and another reviewer for their assistance in evaluating this paper. References Ambrosiano, J., W. H. Matthaeus, M. L. Goldstein, and D. Plante (1988), Test particle acceleration in turbulent reconnecting magnetic fields, J. Geophys. Res., 93, 14,383 – 14,400. Asano, Y., et al. (2006), Detailed analysis of low-energy electron streaming in the near-Earth neutral line region during a substorm, Adv. Space Res., 37, 1382 – 1387, doi:10.1016/j.asr.2005.05.059. Baker, D. N., T. I. Pulkkinen, V. Angelopoulos, W. Baumjohann, and R. L. McPherron (1996), Neutral line model of substorms: Past results and present view, J. Geophys. Res., 101, 12,975 – 13,010. Balogh, A., et al. (2001), The Cluster Magnetic Field Instrument: Overview of in-flight performance and initial results, Ann. Geophys., 19, 1207 – 1217. Borg, A. L. (2006), A study of magnetic reconnection events observed by the Cluster satellites in the Earth’s magnetotail, Ph.D. thesis, Plasma and Space Phys. Group, Univ. of Oslo, Oslo, Norway. Drake, J. F., M. A. Shay, W. Thongthai, and M. Swisdak (2005), Production of energetic electrons during magnetic reconnection, Phys. Rev. Lett., 94, doi:10.1103/PhysRevLett.94.095001. Drake, J. F., M. Swisdak, H. Che, and M. A. Shay (2006), Electron acceleration from contracting magnetic islands during reconnection, Nature, 443, 553 – 556, doi:10.1038/nature05116. Eastwood, J. P., et al. (2007), Multi-point observations of the Hall electromagnetic field and secondary island formation during magnetic reconnection, J. Geophys. Res., 112, A06235, doi:10.1029/2006JA012158. Haaland, S., B. U. Sonnerup, G. Paschmann, M. W. Georgescu, E. Dunlop, A. Balogh, H. Klecker, B. Réme, and A. Vaivads (2006), Discontinuity analysis with cluster, in Cluster and Double Star Symposium, 5th Anniversary of Cluster in Space, 19 – 23 September 2005, edited by K. Fletcher, p. 12, Eur. Space Agency, Noordwijk, Netherlands. Hoshino, M., and T. Mukai (2002), Suprathermal electrons during magnetic reconnection: Fermi model, Adv. Space Res., 30, 1639 – 1644. Hoshino, M., T. Mukai, T. Terasawa, and I. Shinohara (2001), Suprathermal electron acceleration in magnetic reconnection, J. Geophys. Res., 106, 25,979 – 25,998, doi:10.1029/2001JA900052. Imada, S., M. Hoshino, and T. Mukai (2005), Average profiles of energetic and thermal electrons in the magnetotail reconnection regions, Geophys. Res. Lett., 32, L09101, doi:10.1029/2005GL022594. Imada, S., R. Nakamura, P. W. Daly, M. Hoshino, W. Baumjohann, S. Mühlbachler, A. Balogh, and H. Rème (2007), Energetic electron acceleration in the downstream reconnection outflow region, J. Geophys. Res., 112, A03202, doi:10.1029/2006JA011847. Johnstone, A. D., et al. (1997), PEACE: A Plasma Electron and Current Experiment, Space Sci. Rev., 79, 351 – 398. Manapat, M., M. Øieroset, T. D. Phan, R. P. Lin, and M. Fujimoto (2006), Field-aligned electrons at the lobe/plasma sheet boundary in the mid-todistant magnetotail and their association with reconnection, Geophys. Res. Lett., 33, L05101, doi:10.1029/2005GL024971. A07S30 Nagai, T., I. Shinohara, M. Fujimoto, M. Hoshino, Y. Saito, S. Machida, and T. Mukai (2001), Geotail observations of the Hall current system: Evidence of magnetic reconnection in the magnetotail, J. Geophys. Res., 106, 25,929 – 25,950, doi:10.1029/2001JA900038. Øieroset, M., R. P. Lin, T. D. Phan, D. E. Larson, and S. D. Bale (2002), Evidence for electron acceleration up to 300 keV in the magnetic reconnection diffusion region of Earth’s magnetotail, Phys. Rev. Lett., 89(19), 195,001, doi:10.1103/PhysRevLett.89.195001. Rème, H., et al. (2001), First multispacecraft ion measurements in and near the Earth’s magnetosphere with the identical Cluster ion spectrometry (CIS) experiment, Ann. Geophys., 19, 1303 – 1354. Sarris, E. T., S. M. Krimigis, and T. P. Armstrong (1976), Observations of magnetospheric bursts of high-energy protons and electrons at approximately 35 Earth radii with Imp 7, J. Geophys. Res., 81, 2341 – 2355. Sato, T., H. Matsumoto, and K. Nagai (1982), Particle acceleration in time-developing magnetic reconnection process, J. Geophys. Res., 87, 6089 – 6097. Shinohara, I., T. Nagai, M. Fujimoto, T. Terasawa, T. Mukai, K. Tsuruda, and T. Yamamoto (1998), Low-frequency electromagnetic turbulence observed near the substorm onset site, J. Geophys. Res., 103, 20,365 – 20,388, doi:10.1029/98JA01104. Sonnerup, B. U. Ö. (1979), Magnetic field reconnection, in Solar System Plasma Physics, vol. III, edited by C. F. Kennel, L. T. Lanzerotti, and E. N. Parker, pp. 45 – 108, North Holland, Amsterdam. Sonnerup, B. Ö., and L. J. Cahill (1967), Magnetopause structure and attitude from Explorer 12 observations, J. Geophys. Res., 72(1), 171 – 183. Sonnerup, B. U. Ö., G. Paschmann, I. Papamastorakis, N. Sckopke, G. Haerendel, S. J. Bame, J. R. Asbridge, J. T. Gosling, and C. T. Russell (1981), Evidence for magnetic field reconnection at the Earth’s magnetopause, J. Geophys. Res., 86, 10,049 – 10,067. Taylor, M. G. G. T., et al. (2006), Cluster encounter with an energetic electron beam during a substorm, J. Geophys. Res., 111, A11203, doi:10.1029/2006JA011666. Vasyliunas, V. M. (1975), Theoretical models of magnetic field line merging, Rev. Geophys. Space Phys., 13, 303 – 336. Wilken, B., et al. (2001), First results from the RAPID imaging energetic particle spectrometer on board Cluster, Ann. Geophys., 10, 1355 – 1366. A. Åsnes, C. P. Escoubet, H. Laakso, and M. G. G. T. Taylor, ESTEC, Keplerlaan 1, Postbus 299, NL-2200AG, Nordwijk, Netherlands. (aasnes@ rssd.esa.int; [email protected]; [email protected]; [email protected]) A. L. Borg, Norwegian Defence Research Establishment, P.O. Box 25, N-2027 Kjeller, Norway. P. Daly, Max-Planck Institute of Solar System Research, Max-Planck-Str. 2, D-37191 Katlenburg-Lindau, Germany. ([email protected]) A. N. Fazakerley, Mullard Space Science Laboratory, Holmbury St. Mary, Dorking RH5 6NT, UK. ([email protected]) R. W. H. Friedel and B. Lavraud, Los Alamos National Laboratory, MS D466, Los Alamos, NM 87545, USA. ([email protected]; [email protected]) 11 of 11
© Copyright 2026 Paperzz