When the wavelength is less than 8400 Å, the atmospheric absorption lines
are strong and must be eliminated. In order to do this
each spectrum was divided by an atmospheric spectrum. The sky
absorption spectrum was taken as equal to
.
Where
is the normalized sky absorption spectrum obtained from
the standard early type stars. AM and
are the air mass of the star and
standard star respectively. Because of variations of water
vapor density in the earth's atmosphere (i.e.
is variable),
we take a
value near 1 and make several attempts for each
spectrum observed until the resulting spectrum is satisfactory.
Observing run | Date | Telescope | Band | Dispersion | Resolution |
1 | 1992.6.12-6.15 | 1.93 m | 8100-8630 Å | 33 Å/mm | 2.0 Å |
2 | 1993.5.30-6.1 | 1.93 m | 8100-8740 Å | 33 Å/mm | 2.0 Å |
3 | 1996.5.29-5.30 | 2.16 m | 8380-9400 Å | 50 Å/mm | 3.5 Å |
4 | 1997.7.13 | 2.16 m | 7900-9000 Å | 50 Å/mm | 3.5 Å |
5 | 1997.11.7-11.8 | 2.16 m | 8000-9000 Å | 50 Å/mm | 3.5 Å |
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