The model calculations in this study are, as mentioned earlier, inspired by the work of Brandt et al. (1994). The concept is to simulate differential observations of the CMBR with contaminating foreground sources on a single-pixel basis, to add realistic instrument noise and then try to recover the original model parameters by using a non-linear least-squares spectral fitting technique.
By doing so, one should be able to address the very important issue of how well PLANCK and other mission concepts will be able to extract the anisotropies in the CMBR in the presence of hampering foregrounds.
A number of simplifying assumptions are made both with respect to the instrument, the simulated observations and in the actual fitting process. These assumptions, the models and the fitting are described below:
The following contaminating foregrounds are included in the
simulated observations: Synchrotron radiation, free-free emission
and galactic dust emission. The total model used to produce the simulated observations is given by:
where
![]() | = | ![]() |
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The parameters and parameter ranges for the foregrounds,
originally adapted from Fig. 2 (click here) in Bennett et al. (1992), are given below
with GHz and all intensities given in units of 10-20 erg
s-1 cm-2 Hz-1 sr-1.
Synchrotron radiation:
![]() | = | -0.93 |
![]() | = | 0.89 |
![]() | = | ![]() |
![]() | = | ![]() |
Free-free emission:
![]() | = | -0.12 |
![]() | = | 2.11 |
![]() | = | ![]() |
![]() | = | ![]() |
![]() | = | 3.43 |
![]() | = | 3.72 |
![]() | = | ![]() |
![]() | = | ![]() |
Dust emission:
![]() | = | 0.3 |
![]() | = | ![]() |
These estimates of the parameter coverage are made by using various all-sky maps and extrapolating the intensities produced by the parameter ranges given above to these maps thus estimating the sky coverage.
For the synchrotron radiation the Haslam et al. (1982) map was used and for
the dust emission the DIRBE 240 m map used. Since no direct map of the
galactic free-free emission exists the assessment of the free-free coverage
was made using the relation between H
and free-free emission discussed
by Reynolds (1992) and Bennett et al. (1992).
For each model a set of parameters (,
,
,
,
and either
and
or
depending on the dust model) is chosen randomly staying
within the limits listed above and sketched in Fig. 1 (click here).
Using Eq. (5) the observed
differential intensity,
, is then calculated for each
frequency band.
The recovery of the model parameters was performed by fitting a function similar to Eq. (5) to the simulated observations. The fitting was performed using the programme ADAPTION (Brosa 1994) for non-linear least squares fitting. This programme uses Gauss' method for least squares fitting as described by e.g. Press et al. (1989) whereas Brandt et al. (1994) use the Levenberg-Marquardt method (also described by Press et al. 1989). As Brandt et al. (1994) we have taken great care to prevent local minima from contaminating our results.
Important assumptions regarding the fitting are made:
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For the case where the dust is modelled with a two-temperature component
model is given by:
Note the 1 K difference in the coldest dust temperature between the simulated
observations and the model fitted to the data.
In order to get a statistical sample 100 different models are calculated
and the difference between the input parameters
(, (
+
),
,
and
or
) and the fitted parameters
(
,
,
and
and
or
)
are registered (e.g.
). From these differences
means and standard deviations are calculated.