Every scan was bracketed by boresight calibrations. We use a linear interpolation from these to obtain an amplitude and phase correction for each point on the scan.
The boresight observations therefore give us an indication of the data quality. Figures 1 and 2 show the calibration data for each map. Both are excellent.
The phase/time trends are dominated by the satellite motion, seen with
an East-West interferometer of
200m baseline.
(The satellite movement was
0.05 degrees
in azimuth over the course of the observation).
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