![]() |
Figure 1:
a) The scanning of the
polarized detectors provides the measurements of intensity of the CMB field components along four directions at each point on the scan path. b) Definition of axis specifying the Stokes parameters reference frame as seen from the sky. The detector pair on the left
(e.g. 143-4) measures the Q Stokes parameter, while the pair on the right (e.g. 143-2) measures U when Q and U are defined with respect to the
![]() |
Open with DEXTER |
![]() |
Figure 2: Planck focal plane unit (FPU) with polarization sensitive bolometers as seen from the sky. Complementary pairs of PSB detectors are arranged in two horns following each other while scanning the sky so that four detectors are in an optimized configuration for polarization measurement. |
Open with DEXTER |
![]() |
Figure 3:
Broad-band power patterns (
![]() |
Open with DEXTER |
![]() |
Figure 4:
a) Input and recovered B mode power spectrum with an
ideal instrument, i.e. when four identical and axially
symmetric Gaussian beams are used for both the readout generation
and the Cl reconstruction. The small peak at ![]() ![]() |
Open with DEXTER |
![]() |
Figure 5: Histogram of the biases divided by the statistical dispersion for all multipole bins shown in Fig. 4. As expected, the histogram is well fitted by a Gaussian of unit variance, showing that the dispersion on 450 simulations gives a good estimate of the errors. |
Open with DEXTER |
![]() |
Figure 6: Input and recovered power spectra of a) temperature and b) T-E correlation signals, using the simulated beams of Sect. 2 for the readout simulation and the Cl reconstruction. The recovered power spectra are corrected for an average symmetric beam effect by multiplying them by the power spectrum of the average beam map. |
Open with DEXTER |
![]() |
Figure 7: Input and recovered power spectra of a) E mode and b) B mode signals, using the simulated beams of Sect. 2 for the readout simulation and the Cl reconstruction. The recovered power spectra are corrected for an average symmetric beam effect by multiplying them by the power spectrum of the average beam map. |
Open with DEXTER |
![]() |
Figure 8: Recovered B mode power spectrum in a simulation with no initial B mode. The theoretical B mode power spectra due to primordial gravitational waves are also shown for different values of the tensor-to-scalar ratio: 0.1, 10-3, 10-5 and 10-6from top to bottom. |
Open with DEXTER |
![]() |
Figure 9: Spurious generation of E and B modes from temperature signals using simulated beams of Sect. 2 for the readout simulation and the Cl reconstruction, but with no initial E mode. |
Open with DEXTER |
![]() |
Figure 10: Recovered B mode power spectrum before (red, dashed line) and after (green, dot-and-dashed line) correction. The power spectrum is corrected by subtracting the estimated leakage (blue dotted line) assuming knowledge of the exact beams (see text). Bottom: difference between corrected and initial power spectra. |
Open with DEXTER |
![]() |
Figure 11: Recovered B mode power spectrum before (red, dashed line) and after (green, dot-and-dashed line) correction. The power spectrum is corrected by subtracting the estimated leakage (blue dotted line) using beams averaged within one horn (0.5% error, see text). Bottom: difference between corrected and initial power spectra. |
Open with DEXTER |
![]() |
Figure 12: Recovered B mode power spectrum before (red, dashed line) and after (green, dot-and-dashed line) correction. The power spectrum is corrected by subtracting the estimated leakage (blue dotted line) using elliptic Gaussian beams fitted on the exact beams (2% error, see text). Bottom: difference between corrected and initial power spectra. |
Open with DEXTER |