Ozone absorption bands in the 3100 A-3400 A region

Details Ozone absorption bands in the 3100 A-3400 A region Ozone absorption bands in the 3100 A-3400 A region

May 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991pasp..103..457s&link_type=abstract

Astronomical Society of the Pacific, Publications (ISSN 0004-6280), vol. 103, May 1991, p. 457-460. Research supported by Califo

Physics

Geophysics

15

Absorption Spectra, Ozonosphere, Ultraviolet Spectroscopy, Stellar Spectra, White Dwarf Stars

Scientific paper

The physical processes which produce terrestrial ozone absorption are discussed deriving ozone opacities from laboratory cross sections and published ozone column densities. The ozone opacity decreases from about 1 at 3100 A to about 0.001 at 3500 A. A comparison of model DA white-dwarf spectra absorbed by ozone and actual observed spectra shows good agreement. Therefore, simulated absorbed spectra may be used to remove ozone contamination in ground-based data.

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