Astronomy and Astrophysics – Astronomy
Scientific paper
Dec 1980
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980icar...44..640p&link_type=abstract
Icarus, vol. 44, Dec. 1980, p. 640-650. Research supported by the Centre National d'Etudes Spatiales and Institut National d'As
Astronomy and Astrophysics
Astronomy
4
Atmospheric Scattering, Photodissociation, Radiation Absorption, Solar Radiation, Stratosphere, Sulfur Dioxides, Venus Atmosphere, Albedo, Carbon Dioxide, Hydrogen Sulfide, Luminous Intensity, Ozone, Solar Flux
Scientific paper
In the Venusian stratosphere, the available luminous flux which locally produces the photodissociation processes at a given altitude may be divided into three parts: direct incoming downward flux, flux resulting from reflection on cloud surfaces, and flux resulting from molecular scattering. A relatively simple method has been used to calculate the relative importance of these three parts at altitudes between 65 and 100 km. It is shown that the extra contribution of the reflected and scattered fluxes to photodissociation processes cannot be neglected in the UV and visible regions. In the case of SO2, which presents an absorption band in the UV, the photodissociation coefficient is increased 30 per cent due to these effects. Calculations of the photodissociation coefficients of CO, O3, H2S, and SO2 are presented
Moreels Guy
Parisot J.-P.
Zucconi Jean-Marc
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