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Astron. Astrophys. 336, 769-775 (1998) 2. Observations and data reductionThe observations were performed with the 1.23 m telescope on Calar
Alto Observatory, Spain between the 3rd and 14th of April 1997,
comprising 6 days with acceptable observational conditions. We
recorded time series with a duration of at least one hour and a
temporal resolution of 20 and 30 seconds using a Gunn g and a
Strömgren v filter. A total field of view of
Table 1. Overview on the obtained data sets Two different sources contribute to the observed intensity signal: reflected sunlight and stimulated emission by resonant fluorescence. Thus the signal might be influenced by an oscillating solar wind (changes of density and of the magnetic field) but also by genuine activity of the comet (like changes in evaporation, and by effects of rotation). In addition, the signal might be affected by changes in the earth's atmosphere, by straylight, and by instrumental effects. For the distinction of different processes, we alternated between two different filters in subsequent nights. Both filters transmit photons from stimulated emission and reflected sunlight, but with different contributions. We used a broad filter (Gunn g) to detect reflected sunlight and a narrow filter (Strömgren v) centered on a molecular spectral line (namely C3 at 4100 Å). Fig. 2 shows the corresponding transmission curves. Unfortunately, all hitherto published spectra of Hale-Bopp taken in the appropriate frequency band were observed at rather large heliocentric distance (e.g. Fig. 2 in Fitzsimmons & Cartwright 1996 at 6.82 AU and Fig. 1 in Cartwright 1997 at 4.2 AU). Instead we use here a spectrum of comet Hyakutake (ESO Press Photo 22/96) taken at a heliocentric distance of about 1 AU. This spectrum was used to prepare the observations of Hale-Bopp, assuming a general similarity of the spectra of both comets.
© European Southern Observatory (ESO) 1998 Online publication: July 20, 1998 ![]() |