The sky absorbtion is estimated from the variability of the average flux
of the bright star used for seeing measurements. This parameter is easy to compute because it does
not involve airmass correction, neither zero point estimate. Moreover, it appears that, over 10mn time
bins and neglecting source chromaticity effects, the relative rms flux variation is about
identical to the rms of the extinction coefficient, in R magnitude per
airmass. A study of the extinction coefficient
shows cases of correlation with local meteorology.
The graph shows the correlation between the relative rms flux variation and the rms of the extinction
coefficient for the month of June 2000 at La Silla. The extinction coefficient is determined by
aperture photometry relative to an arbitrary reference corresponding for each star to the best
conditions of the month. The method induces an error (false alarm) on the determination of non
photometric sky less than 7% of the time with a 10% margin, and only 2% of the time with a 20%
margin
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