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Figure 1:
Relations between the heliocentric and cloud-centred frames used to
describe the Solar System scanning geometry for a mission like PLANCK.
The relations between Planck, Sun, Cloud Center and the observed portion of cloud are drawn,
the L2 point is not drawn to simplify the graph. The connection between the other two reference frames is shown in Fig. 2.
An example of scan circle and the related spin axis,
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Figure 2:
Relations between the cloud-centred ecliptic reference frame,
the cloud symmetry reference frame and the spacecraft
centred corotating reference frame.
Top panel: angles between the cloud-centred Ecliptical reference
frame (full yellow disc (light-gray in the bw version) - black arrows),
and the cloud cylindrical symmetry reference frame (dashed blue disc - red arrows).
Bottom panel: angles between the cloud cylindrical symmetry reference
frame, the cloud-centred corotating cylindrical reference frame,
the spacecraft - centred corotating reference frame.
The displacement of PLANCK (in this case above the symmetry plane),
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Figure 3:
Simulated contour plot of
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Figure 4:
Simulated data stream of surface brightnesses (MJy/sr) measured at
857 GHz for the ZLE - smooth component (red), the Galaxy (green)
and the sum of the two (blue). The ordinate is the phase of the scan circle, assumed to be zero for the pointing direction nearest to the North ecliptic Pole. Two subsequent scan circles are displayed, the phase of the second being augmented of ![]() ![]() |
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Figure 5:
Relative contribution of ZLE, Galactic (dust) emission and noise as a function
of the pointing ecliptical longitude at three PLANCK frequency bands: 857 GHz ( top),
545 GHz ( middle), 343 GHz ( bottom).
For each pointing ecliptical longitude, the plots gaves the ratio of the
ZLE over the Galactic emission
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Figure 6:
Derivatives of
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Figure 7:
Absolute and relative variation of the ZLE surface brightness during the
year at 857 GHz. The full-red line (light-gray in bw) is the yearly averaged ZLE surface brightness [MJy/sr] for a given eclipitical latitude.
The surrounding green band (dark-gray in bw) is the variation of ZLE surface brightness
during the year. Below (full black lines) the relative variation (with respect to the average)
of ZLE for a set of representative longitudes (from the left of the
black curves, from ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
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Figure 8:
Seasonal modulation of the Smooth component of the ZLE at 857 GHz
for four selected pointing directions: the North ecliptic Pole (N),
the South eclitptic Pole (S), the Forward direction with respect to the PLANCK motion (FW) and
the Backward direction (BW). Longitudes are relative to the longitude of the ascending node.
Upper frame: the surface brightness variation looking to N (full line), S (long dashed line), FW (short dashed line), BW (dot-dashed line). The variation is the difference
between the surface brightness along the direction of choice and its yearly average. Here
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Figure 9:
Deviation of the ZLE from an f2 scaling as a function of
the direction in the sky. Upper frame: the original data for f = 100, 143, 217,
353, 545, 857 GHz (from lower to upper surface brightness).
Lower frame: deviation from the f2 scaling in terms
of
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Figure 10:
Map of
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Figure 11:
Differential surface brightness of the ZLE from the Smooth component in
the 857 GHz channel,
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Figure 12:
Effect of the random relative calibration error on the Ef determination
with the differential method at 857 GHz for 2![]() ![]() ![]() ![]() |
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