For sake of clarity,
we have first
performed our simulations neglecting the galactic emission
in order to obtain general results holding for low
foreground regions.
A flat CDM model with H0=50 km/s/Mpc and a baryon density in terms
of critical density , with a 24% of mass in Helium,
has been adopted for the present
tests, but some other models have been considered for comparison
(see Sect. 4.7).
For the standard Planck scanning strategy, a test on a given
scan circle consists of about
680 integrations at 30 GHz and of about 1700 integrations
at 100 GHz.
We can estimate the numerical error introduced by interpolation
and integration techniques by comparing for few cases
the results obtained by using an integration
grid of
points with those obtained with a grid
of
points (see Col. 8 of Table 1).
We have firstly performed our tests using maps at a resolution of about 5' (COBE-cube resolution 11). Figures 2 and 3 show our results for a typical test at 30 GHz and at 100 GHz respectively. Even in correspondence of the largest temperature variations induced by CMB quadrupole large scale waves, the temperature differences remain practically equal to those obtained in other sky regions (see the bottom panels of Figs. 2 and 3).
Typical results
obtained
by using maps at COBE-cube resolution R=11
are tabulated in Table 1 (tests 1-6) in terms of for
different beam FWHM's and distortion parameters r.
Column 8 in Table 1 gives the numerical error,
,in the determination
of
derived from
the comparison of results obtained for a typical scan circle with
a symmetric beam by using different integration grids (of course
the reported value of
is
times
that derived from this test).
These results may be qualitatively interpreted from a geometrical point of view: the contribution of the different parts of the sky observed by beams with different shapes becomes more important and produces a growing effect as the FWHM and/or r increases (Burigana et al. 1997).
On the other hand we may expect that these
results depend in part on the resolution of the maps used for the test.
Indeed the use of maps at lower resolution tends to smear out
the differences of temperature between different pixels and we
expect that the value of
may decrease by passing from higher to lower resolution maps, as confirmed
by the results of the test 7 in Table 1, performed by using
the same map at 30 GHz of the above tests but degraded at
a lower resolution (see Sect. 4.4).
The results of the previous section indicate that mainly depends
on three quantities: the beam distortion parameter, r, the beam
,where the suffix "prime'' indicates that it is expressed in arcminutes, and
the map resolution, R, or equivalently the typical pixel dimension, d.
A simple expression for the beam distortion effect as
function of these parameters can be useful for many purposes.
We will search here for a formula based on the assumption
of separability of the variables, i.e. of the kind:
![]() |
||
(5) |
For understanding the dependence of on the beam FWHM we have
performed
four tests by keeping constant the ratio,
, between
the typical pixel dimension and the beam size,
and the beam distortion parameter r. We have considered
a case with a beam size
somewhat larger than those of Planck LFI
radiometers in order to give results holding also for observations
performed with smaller telescopes.
The corresponding results are tabulated in Table 2 (tests 8-11).
They can be well described by a function f (see left panel of Fig. 4):
![]() |
||
(6) |
For understanding the dependence of on
the ratio
we have carried out
three tests by keeping constant the beam size and the beam
distortion parameter r.
We have choosen a value
which is intermediate
between those relevant for Planck LFI radiometers.
The corresponding results are tabulated in Table 2 (tests 12-14).
They can be well described by a function g (see middle panel of Fig. 4):
![]() |
(7) |
The results
of the tests 1-6 in Table 1 cannot be directly used to estimate the
dependence of the beam distortion effect on the beam distortion parameter
r, being based on maps with different ratios
and different FWHM. On the other hand from Eqs. (6) and (7)
we know how these two parameters may affect the test. Then
we fit the values of
of the tests 1-6 in Table 1
divided by the functions f and g. By including the obvious
condition of null distortion effect in the case r=1, for the
function h we obtain the simple expression (see right panel of Fig. 4):
![]() |
(8) |
![]() |
||
(9) |
This approximation works quite well
for FWHM , as we have verified
by comparing it with the results of Tables 1 and 2
and a few number of other different tests.
Typical errors are about
0.25
and always less than 0.7
and it works even better
for
(typical errors less than 0.1
).
We note that tests based on sky maps directly simulated
at low resolution, and not obtained from degradation
of high resolution maps, tend to show a somewhat larger effect
(for example about 30% greater for R=9).
In the asymptotic case of maps at very high resolution
(
)we can neglect the dependence on d, by setting g=1, and replace the
proportionality constant with
in Eq. (9).
The above results are obtained by exploiting a simulated sky map
in the case of pure CDM model for CMB fluctuations.
We have performed other tests with different cosmological scenarios.
We have considered the case of a beam with a FWHM of 18'
and a
beam distortion parameter r=1.3 for two maps
directly generated at resolution R=10
obtained for a flat MDM model (,
,
, H0=50 km/s/Mps)
and for a flat
CDM model (
,
,
, H0=50 km/s/Mps).
We have
and 1.74
respectively, in good
agreement with the results of Sect. 4.6.
Although the accurate study of the effect of beam distortions
when the telescope rotation around the satellite spin axis
is taken into account is far from the purposes
of the present work, we consider here that
the Planck sampling scheme assumes 3 samplings per FWHM.
During this time the telescope continuously changes its pointing
direction; we have carried out a simulation neglecting the telescope
motion within a single sampling time,
but assigning to each of the 3 samplings a different telescope direction,
so roughly considering the telescope motion
during the integration time.
We simply compare the average of three samplings obtained by
a symmetric beam with that obtained by an elliptical one.
When we compute the differences between these two data streams for
a typical scan on a pure CMB fluctuation map
for a distortion parameter r=1.3 (the case
of the test 2) we obtain a value of
,just a little lower than that found for the test 2.
This test indicates
that the oversampling of
the sky introduced by the telescope motion cannot be used
in simple way to significantly reduce the effect of main beam distortions on
anisotropy measurements, as intuitively expected from the fact
that during an integration time does not change significantly
the orientation of a distorted beam respect
to the observed sky region.
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