Polarization induced by cosmological scalar perturbations leads to a t
ypical anisotropy pattern, which can best be analyzed in a Fourier dom
ain. This allows one to distinguish a cosmological signal of polarizat
ion unambiguously from other foregrounds and systematics, as well as f
rom polarization induced by nonscalar perturbations. The precision wit
h which polarization and cross-correlation power spectra can be determ
ined is limited by cosmic variance, noise, and foreground residuals. T
he choice of estimator can significantly improve our capability of ext
racting a cosmological signal, and in the noise-dominated limit the op
timal power spectrum estimator reduces the variance by a factor of 2 c
ompared to the simplest estimator. If foreground residuals are importa
nt, then a different estimator can be used, which eliminates systemati
c effects from foregrounds so that no further foreground subtraction i
s needed. A particular combination of Stokes Q and U parameters vanish
es for scalar-induced polarization, thereby allowing a direct determin
ation of tensor modes. Theoretical predictions of polarization in stan
dard models show that one typically expects a signal at the level of 5
-10 mu K on small angular scales and around 1 mu K on large scales (l
< 200). Satellite missions should be able to reach sensitivities neede
d for an unambiguous detection of polarization, which would help to br
eak the degeneracies in the determination of some of the cosmological
parameters.