Astron. Astrophys. 356, 418-434 (2000)
3. Testing the method
In order to test our method to determine cosmological parameters
for stability, we have constructed a mock sample of observational
data. We start with a set of cosmological parameters and determine for
them the "observational" data which would be measured in case of
faultless measurements with errors
comparable to the observational errors. We then insert random sets of
starting parameters into the search program and try to find the right
model which corresponds to the mock data. The method is stable if we
can recover our input cosmological model. Even starting very far away
from the true values, our method reveals as very stable and finds the
`true' model whenever possible (see Table 3).
![[TABLE]](img185.gif)
Table 3. Test of the method: results of parameter search from mock data for the tilted MDM model ( , , , , , ). In test 1, all parameters are determined; in the 2nd to 6th tests, some parameters are fixed. For each test the first row corresponds to the case when the number of species of massive neutrinos is equal to the input value (2) and the second - when .
Notes:
*) - fixed parameters.
One of the main ingredients for the solution to our search problem
is a reasonably fast and accurate determination of the transfer
function which depends on the cosmological parameters. We use the
accurate analytical approximations of the MDM transfer function
depending on the parameters
, ,
,
and h by (Eisenstein & Hu 1999 and Novosyadlyj et al.
1999).
The linear power spectrum of matter density fluctuations is
![[EQUATION]](img187.gif)
where A is the normalization constant and
is the linear growth factor, which
can be approximated by (Carroll, Press & Turner 1992)
![[EQUATION]](img189.gif)
where .
We normalize the spectra to the 4-year COBE data which determines
the amplitude of density perturbation at the horizon crossing scale,
(Liddle et al. 1996, Bunn and
White 1997), which for a matter dominated Universe without tensor mode
and cosmological constant is given by
![[EQUATION]](img192.gif)
For a flat model with cosmological constant
( ) we have
![[EQUATION]](img194.gif)
( ). The normalization constant
A is then given by
![[EQUATION]](img196.gif)
The Abell-ACO power spectrum is related to the matter power
spectrum at ,
by the cluster biasing parameter
. We assume a scale-independent,
linear bias:
![[EQUATION]](img199.gif)
For a given set of parameters n,
, ,
h, ,
and
theoretical values of
can now be obtained for the values
of Table 1. We denote them by
( ).
The dependence of the position and amplitude of the first acoustic
peak of the CMB power spectrum on cosmological parameters has been
investigated using CMBfast by Seljak & Zaldarriaga 1996. As
expected, the results are, within sensible accuracy, independent of
the hot dark matter contribution ( ).
This is illustrated in Figs. 4 and 5.
![[FIGURE]](img208.gif) |
Fig. 4. The dependence of the acoustic peak amplitude on neutrino content
|
![[FIGURE]](img214.gif) |
Fig. 5. The dependence of the acoustic peak position on neutrino content
|
For the remaining parameters, n, h,
and ,
we have determined the resulting values
and
with CMBfast for a network of model
parameters. The values in-between
grid points are then obtained by 4-dimensional interpolation. This
allows a fast and sufficiently accurate calculation of the peak
position and amplitude for a given set of parameters in the range
,
,
and considered in this work. The
accuracy of this interpolation is estimated to be within 2%. We denote
and
by
and
respectively.
The theoretical values of the other experimental constraints are
obtained as follows: The density fluctuation
is calculated according to
Eq. (3) with taken from
Eq. (12). We set and
, where
for
and
for
, respectively.
The rms peculiar velocity of galaxies in a sphere of radius
Mpc is given by
![[EQUATION]](img227.gif)
where is the power spectrum for
the velocity field of the density-weighted matter (Eisenstein & Hu
1999), is the top-hat window
function. A previous smoothing of raw data with a Gaussian filter of
radius Mpc is employed here similar
to the procedure which has led to the observational value. For the
scales of interest . We denote the
rms peculiar velocity by .
The value by Gnedin 1998 from the formation of
Ly- clouds constrains the rms linear
density perturbation at and
Mpc. In terms of the power spectrum
is given by
![[EQUATION]](img235.gif)
It will be denoted by . The
corresponding value of the constraint by Croft et al. 1998 is
![[EQUATION]](img237.gif)
at and
, (where
is the Hubble parameter at redshift
z) will be denoted by . The slope of
the power spectrum at this scale and redshift,
![[EQUATION]](img241.gif)
is denoted by .
For all tests except Gnedin's Ly-
clouds we used the density weighted transfer function
from Eisenstein & Hu 1999. For
Gnedin's we use
according to the prescription of
(Gnedin 1998). It must be noted that even in the model with maximal
( )
the difference between and
is less than
for
.
Finally, the values and h
are denoted by and
respectively.
The relative quadratic deviations of the theoretical values from
their observational counterparts are given by
:
![[EQUATION]](img250.gif)
where and
are the experimental data and their
dispersion, respectively. The set of parameters n,
, ,
h, ,
and
or some subset of them can be
determined by minimizing using the
Levenberg-Marquardt method (Press et al. 1992). The derivatives of the
predicted values with respect to the search parameters which are
required by this method are calculated numerically using a relative
step size of with respect to the
given parameter.
The method was tested in the following way. Assuming a 4-year COBE
normalized tilted MDM model with the
parameters ,
,
,
,
,
and assuming further a cluster biasing parameter
we have calculated mock cluster
power spectrum and treated them as
,
. The remaining mock data
,
have been calculated as described above. We have assigned to these
mock data the same relative `experimental' errors as in the
corresponding experiments described in the previous section.
We then used these mock data to search the parameters n,
, ,
h, , and
(
was fixed). As starting parameters for the search program we assumed
random values within the allowed range. We have searched for the
parameters assuming the "true" value of two species of massive
neutrinos as well as assuming three species of massive neutrinos. The
parameters obtained for different cases are presented in Table 3.
The errors in the determined parameters are calculated as root square
from diagonal elements of the standard error covariance matrix. In all
cases the code found all the previous known parameters with high
accuracy. This means that the code finds the global minimum of
independent of the initial values for
the parameters.
Our conclusions from the test results can be summarized as
follows:
1. If all parameters are free and
(the input value) the code finds
the correct values of the free parameters (test 1, for
in Table 3).
2. If all parameters are free and
the code finds values of the free
parameters which are in the range of
errors (test 1, for in
Table 3).
3. If some parameters are fixed and differ from the input values
(tests 2, 4, 6 in Table 3) the code finds for the remaining
search parameters values close to the correct ones. The most stable
and accurate value is . The results
for n, and
are in the
range of the correct values. The
most uncertain solutions are found for n and
if an incorrect value for
has been assumed (test 6 in
Table 3).
4. If some parameters are fixed to the predetermined ones and
(the input value) the code finds
the correct values of the free parameters (test 3 and 5, for
in Table 3), if
the determined values are within
the range (test 3 and 5, for
in Table 3).
In summary, the code determines the parameters n,
, ,
h, and
correctly, if the observational data
are correctly measured and the cosmological model assumed is correct;
i.e. no curvature, a negligible amount of tensor perturbations
and a primordial spectrum of scalar perturbations which is scale free
from the present horizon size down to the scale of the
Ly- clouds.
© European Southern Observatory (ESO) 2000
Online publication: April 10, 2000
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