Anomalous atmospheric spectral features between 300 and 310 nm interpreted in light or new ozone absorption coefficient measurements

Details Anomalous atmospheric spectral features between 300 and 310 nm interpreted in light or new ozone absorption coefficient measurements Anomalous atmospheric spectral features between 300 and 310 nm interpreted in light or new ozone absorption coefficient measurements

Mar 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982georl...9..227m&link_type=abstract

Geophysical Research Letters, vol. 9, Mar. 1982, p. 227-230.

Physics

10

Atmospheric Scattering, Backscattering, Molecular Absorption, Ozone, Spectrum Analysis, Ultraviolet Absorption, Abnormalities, Absorption Spectra, Absorption Spectroscopy, Absorptivity, Atmospheric Radiation, Error Analysis, Satellite Observation

Scientific paper

Real structure is revealed, by an analysis of continuous scan data from the solar backscattered UV instrument on Nimbus 7, in the backscattered atmospheric albedo region between 300 and 310 nm where spectral anomalies have been reported in ground-based observation. The spectral anomalies are explainable as structure at the 1-5% level in the ozone absorption coefficient, as measured by Bass and Paur (1981). The new absorption coefficient measurements are judged to approach the 1%-level of accuracy in atmospheric radiation calculation, which should resolve discrepancies between different Dobson wavelength pairs and between different instruments and permit the more accurate analysis of such second-order effects as NO emission, SO2 absorption in polluted atmospheres, and Raman scattering effects.

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