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Subsections

4 Observations and data reduction

4.1 Observations


  \begin{figure}
\par\includegraphics[width=7cm,clip]{MS2234f2.eps} \end{figure} Figure 2: MuSiCoS 98 observations of $\omega $ Ori with breakdown for each site.

$\omega $ Ori was intensively observed in 1998 from November 23 to December 15 with 8 telescopes (see Table 2 and Fig. 2):


 

 
Table 2: Journal of MuSiCoS 98 observations of $\omega $ Ori.
HJD span(d) Site N. of Exposure S/N
(2451100+)   spectra time (min)  
39.64-47.72 OHP152 33 15-20 200-500
41.42-47.72 OHP193 29 15-20 300-400
41.66-44.93 Kitt Peak 36 15-25 100-200
43.78-60.88 ESO 47 20 100-300
46.29-55.41 Xinglong 22 20 200-300
47.10-51.08 Stromlo 13 10 150-200
48.74-56.65 LNA 27 18-25 300-500
50.66-58.75 INT 36 7-30 50-150


Bias, flat fields and wavelength calibration exposures produced by Th-Ar lamps were obtained every 2-4 hours. An early-type comparison star with low vsini, $\gamma$ Peg, telluric standard stars such as $\alpha $ Peg and velocity standard stars such as $\beta$ Lep were observed from each site to correct for telluric lines and check for possible problems in the calibration.

4.2 Reduction

The instruments lack homogeneity: gratings, filters, ranges of wavelengths in the orders of échelle spectra and detectors are different, which hampered the data reduction procedure. The OHP152, Kitt Peak, LNA, Mount Stromlo and INT data were reduced using IRAF[*] software. The OHP193, ESO and Xinglong data were reduced with MIDAS[*] software. A correction for the motion of the Earth was applied and the telluric lines were removed when possible. Finally each line in each individual spectrum has been normalized by selecting precise continuum points around the line, and rebinned on a carefully chosen equidistant wavelength grid (0.1 Å) using IRAF. The normalization of the spectra is the most critical part of the reduction procedure of multi-site campaigns to obtain homogeneous data (see Hubert et al. 1997).


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