next previous
Up: Nonvariability among Bootis

4. Reductions

All data were corrected for dead time, atmospheric extinction and sky background. In case of observations during more than one night, we merged the data prior to a Fourier analysis. Neither smoothing nor averaging was applied. The differential data were calculated by subtracting one data set from the other. If necessary, we interpolated linearly between two data points of the comparison star for a given time.
The differential data were used to calculate amplitude spectra with a standard Fourier technique (Deeming 1975; Breger 1990) up to the Nyquist frequency as shown in Figs. 4 (click here)a to 4 (click here)c. We have also checked the differential data of both comparison stars for variations.



Copyright by the European Southern Observatory (ESO)
web@ed-phys.fr