Tracking errors
The telescope encoders return values in the azimuth-elevation system,
so the TRACKING_AZ values from the IMBFITS tables must be
multiplied by
in order to have a reliable idea of
the telescope behavior on the sky. The
Figure
shows3.8 three real examples for three different scans. While the
tracking errors seem comparable in both directions at low elevation,
the dispersion in azimuth is completely flatenned near the pole: the
same jittering of the telescope along the azimuth axis results in
different jittering on sky, depending on the elevation
(
). Question: no wind effect near
zenith??
Figure:
Antenna position (blue) and tracking errors (red) of three
drift subscans from three different on-the-fly scans, with two
zoom factors for each. The tracking errors are displayed from a
unique central position in order to visualize the
dispersion in both directions, and a magnification factor is
applied for better visibility. All plots show the
azimuth-elevation sphere under an arbitrary orientation and the
associated grid. Top: On-the-fly scan from the
MRTCAL test data, at about
elevation. Center: On-the-fly scan near the zenith
(
); subscan drifts along right-ascension, nearly
equivalent to elevation scanning for the source and date-time of
observation. Bottom: Same, but scanning along
declination, nearly equivalent to azimuth scanning.
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