Determination of the general ozone abundance from spectrophotometric UV observations of the Sun

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Scientific paper

We describe a new version of the multiwave technique for determinating the total ozone content in Earth's atmosphere. The technique is based on the assumption that the aerosol attenuation depends arbitrarily on wavelength. It was used for the processing of solar spectrophotometric observations in the near-UV region (305-340 nm) in 1989 and 1998 at the High-Altitude Station Terskol of the Main Astronomical Observatory of the Academy of Sciences of Ukraine. The data processing showed that not only the total ozone content could be determined with the technique but a number of other trace gases as well including SO2, NO2, along with the spectral dependence of aerosol absorption.

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