Although no other method has yet been developped specifically for destriping polarized data, many methods exist for destriping unpolarized CMB data, which could be adapted to polarized data as well.
We first comment on the classical method which consists in modelling the measurement as
| (24) |
the noise. The problem is solved by inversion, yielding an estimator of the signal:
| (25) |
This method can be extended straightforwardly to polarized measurements,
at the price of extending by a factor of
the size of the matrix
,
by 3 that of
vector
(replaced by
), and by h that of the data
stream (remember that h is the number of polarimeters).
The implementation of this formally simple solution may turn into
a formidable problem when megapixel maps are to be produced. Numerical
methods have been proposed by a variety of authors
[Wright1996,Tegmark1997], that
use properties of the noise correlation matrix (symmetry,
band-diagonality) and of the pointing matrix (sparseness).
Such methods, however, rely critically on the assumption that the noise is
a Gaussian, stationary random process, which has been a reasonable
assumption for CMB mission as COBE where the largest part of the
uncertainty comes from detector noise, but is probably not so for sensitive
missions such as Planck. Our method requires only inverting a
matrix
where n is the number of circles involved, and does not assume
anything on the statistical properties of low frequency drifts. It just assumes
a limit frequency (the knee frequency) above which the noise can be considered as a white
Gaussian random process.
Another interesting method is the one that has been used by Ganga in the analysis of FIRS data [Ganga1994], which is itself adapted from a method developed originally by Cottingham cottingham87. In that method, coefficients for splines fitting the low temperature drifts are obtained by minimising the dispersion of measurements on the pixels of the map. Such a method, very similar in spirit to ours, could be adapted to polarization. Splines are natural candidates to replace our offsets in refined implementations of our algorithm.
Here, we have assumed that the averaged noise can be modeled as circle
offsets plus white noise (Eq. 8), i.e. that the noise between
different measurements from the same bolometer is uncorrelated after
removal of the offset. This allowed us to simplify the
to
that shown in Eq. (9). In reality, the circular offsets do not
completely remove the low frequency noise and there does remain some
correlation between the measurements. The amount of correlation is
directly related to the value of
;
the smaller
the smaller the remaining correlation.
Figures 13-18
already contain the errors induced from the fact that we did not
include these correlations in the covariance matrix, and thus
demonstrate that the effect is small for
.
Acknowledgements
We would like to acknowledge our referee's very useful suggestions.
Copyright The European Southern Observatory (ESO)