The active control of the CES predisperser and grating provides a very
high wavelength stability that has been repeatedly verified. This
stability implies that for many scientific programmes it is not necessary
to take repeated wavelength calibrations during the night. Whether or not
wavelength calibrations should be repeated depends, of course, on the
specific requirements of the user for calibration accuracy. To aid this
decision the typical variation of the central wavelength on the CCD is
illustrated here.
Measured at 5400 Å a variation of only 0.05 pixels rms or 0.2 pixels
peak-to-peak is seen in the course of a 10 hour night.
This corresponds (at the given wavelength) to a variation in radial
velocity units of only 25 m/s rms or 100 m/s peak-to-peak.
The upper figure shows the wavelength drift behaviour
in units of CCD pixels (y-coordinate is direction of dispersion)
as measured during one night.
Observers should note in any case that La Silla observatory receives weak
Earth quakes quite frequently which can occasionally lead to wavelength
shifts larger than demonstrated here.
In the direction perpendicular to the dispersion (x-coordinate on the CCD)
larger shifts of up to
1 - 5 pixels have been measured. An example is shown in the
second figure.
See the monitoring pages for recent results.
These shifts correspond to a non-negligible fraction of the width of
individual slices with
consequences for the performance of flatfielding.
If possible, it is recommended to take repeated sets of flatfield
exposures during the night. At any rate before using the flatfields
in the data reduction process they should be normalized, e.g. divided
by their average profile.
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