Dark Energy as an Inverse Problem Cristina España i Bonet1 and Pilar Ruiz-Lapuente2 Departament d'Astronomia i Meteorologia, Universitat de Barcelona, Martí i Franquès 1, E-08028 Barcelona, Catalunya, Spain 1 2 [email protected] [email protected] Abstract Inverse Problem The aim of an inverse problem is to determine the values of a set of parameters appearing in a theoretical expression from a set of observables. So studying dark energy using this approach is an inverse problem. For the linear discrete case the solution of an inverse problem can be solved via the least squares method, but for nonlinear and/or continuos cases the method must be generalized. The version used here is a Bayesian approach to this generalization [1]. We consider a flat universe with only two dominant constituents (at present): cold matter and dark energy. Therefore we characterize the cosmological model by the density of matter, ΩM, and by the parameter w(z) of the equation of state of the dark energy. In order to improve the information on dark energy it is not only important to have a large number of data of a good quality, but also to know where are these data more profitable and then explode all the statistical methods to extract the information. We apply here the Inverse Problem Theory to determine the parameters appearing in the equation of state (EoS) and the functional form itself. Using this method it is also determined which would be the best distribution of high redshift data to study the equation of state of dark energy, i.e., with which distribution it is obtained a best quality of the inversion. Supernovae magnitudes are used alone and together with other sources such as radio galaxies and compact radio sources. Data The main data used in this work are SNe Ia at high redshift [2] although we also consider other sources at even higher z such as radio galaxies (RG) [3] and compact radio sources (CRS) [4]. In order to join all these data it is useful to define the dimensionless coordinate distance y as [5]: yi ≡ mi − M 5 zi 10 dz ' , =∫ 3 c(1 + zi ) 0 Ω (1 + z ') + Ω ( z ' ) M X σy = i ( Continuous case Just as in the discrete case there is an iterative equation to obtain the EoS. The difference now is that it can be calculated at every desired redshift: ) ln 10 yi σ mi + σ M . 5 Using the Inverse Problem Theory to determine the discrete parameters appearing in an EoS of the form i =1 0 Where Cw is the covariance function, g is the kernel of the derivatives and W is the same vector as before. z 1+ z w(z) = w0 + wa we have obtained an iterative value for ΩM, w0 and wa [6]: ∂yith Wi ∑ ∂Ω M i =1 This way we don’t have to make any hypothesis about the specific form of the EoS, but the price to pay is the introduction of a priori information. N 2 ΩM w0[ k +1] th ∂ y = w00 + σ w20 ∑ Wi i ∂w0 i =1 wa[ k +1] ∂yith = w + σ ∑ Wi ∂wa i =1 N N 0 a zi w[ k +1](z) = w0 ( z ) + ∑ Wi ∫ C w ( z , z ' ) g w ( z , z ' )dz ' Discrete Case Ω M [ k +1] = Ω M 0 + σ N 2 wa The table shows the results with the different sources used and combinations of them. Next to each parameter there is the mean index I, a very useful parameter defined to see how the data restrict the model, being the ideal case that with I =1. Data of SNe Ia alone are the best ones to determine the EoS, but the results can be improved up to a 50% with the inclusion of these other sources at higher redshift. Current data slightly favour an EoS near the one of a cosmological constant but allowing a positive evolution. The left panel shows the results with data coming from de gold set of [2]. Top figure represents the evolution of the EoS with the 1σ intervals when it is assumed an a priori value of w(z)=-1±1 and the density of matter is fixed to ΩM=0.3. So, a cosmological constant is compatible with current SNe Ia data. The lower panels are used to see the reliability of the result. The resolving kernel K(z,z’) informs about how well determined is the redshift z’ . Low redshifts are better determined, as there is a larger number of data, and it is reflected with a sharper K(z,z’). The mean index I(z) has the same interpretation as in the discrete case, and such low values indicate that the results can only be trust when the a priori is totally justified. Estimating the best distribution of data Nowadays several experiments are being designed in order to detect new sets of SNe Ia at high redshift. It is then important to know where should be these data concentrated to determine with a minimum error the parameters appearing in the EoS. We need then the best distribution, i.e., the distribution which gives the best result. In order to quantify this quality we will ask for two characteristics in the result: it must have a small uncertainty (precision) and the best value must be near the “true” one (accuracy). As we are going to simulate gaussian distributions of data, the “true” value will be the “seed” of the simulation. So, we define the quality factor as 1 1 . , Qw0 = log Qwa = log seed seed σ w w0 − w0 σ w wa − wa 0 a Conclusions The results are shown in the figure on the right. Zones with dark blue represent distributions with the highest quality of the inversion, whereas the lightest zone are those with a bad quality, as shown in the colour scale next to the figures. It has been applied the method of resolution of inverse problems to the dark energy equation of state. The column shows the results for a fiducial model of CC (w0=-1, wa=0) inverted using these “seed” values as a priori. In general, we observe that all the distributions determine much better w0 than wa. Furthermore, distributions centred only at high redshift give very poor results even for wa. When we join together the qualities in both parameters we see more clearly that there is another poor section at low redshift with a small width. So, we see the necessity to extend the number of data at high redshift. This has been already done within the GOODS and HST Treasury Program [7] for example, and must be continued and extended in order to be in the best condition to study dark energy. Alternatives to a CC are considered in the top row where it is shown a SUperGRAvity model (w0=-0.8, wa=0.6) and a similar one with (w0=-0.8, wa=-0.3). Nowadays SNe Ia data and this method determine w0 with a relative error of ~30% and wa with one of ~100%, depending the exact value on the number of studied parameters. References [1] A. Tarantola and B. Valette, Rev. Geophys. & Space Phys., 20(2), 219 (1982). [2] A.G. Riess et al., Astrophys. J., 607, 665 (2004). [3] R.A. Daly and S.G. Djorgovski, Astrophys. J., 612 (2004). [4] L.I. Gurvits et al., Astron. Astrophys., 342, 378 (1999). [5] R.A. Daly and S.G. Djorgovski, Astrophys. J., 597, 9 (2003). [6] C. España-Bonet and P. Ruiz-Lapuente, in preparation. Adding other sources at high z such as RG and CRS reduces these errors in almost a 50%. As with SNe Ia alone, the high mean index indicates a very good inversion and a high reliability on the results. The inverse method can also be applied to determine the function w(z) itself. A pure cosmological constant can not be discarded from these results. In this case the low mean index demands using a very well motivated priors. A gaussian distribution of SNe Ia centred at z0~0.7 with a width of σz~1 would give us the best determination of w0 and wa. [7] http://www.stsci.edu/science/goods Photo courtesy of Nik Szymanek and Ian King for the Isaac Newton Group of Telescopes
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