Ozone on Mars - The effects of clouds and airborne dust

Physics

Scientific paper

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Abundance, Atmospheric Chemistry, Dust, Mars Atmosphere, Ozone, Aeronomy, Opacity, Photochemical Reactions, Photodissociation, Polar Regions, Reaction Kinetics, Mars, Ozone, Clouds, Dust, Atmosphere, Photochemistry, Polar Regions, Latitude, Abundance, Opacity, Photodissociation, Absorption, Aeronomy, Seasonal Variations, Reflectance, Spectroscopy, Models, Scattering, Spacecraft Observations, Mariner 9 Mission

Scientific paper

Photochemistry in the winter polar atmosphere of Mars is examined for several latitudes, cloud types and dust abundances. Variations in cloud opacities and cloud types change O3 abundances only a few percent. However, typical dust abundances induce 10 - 50% increases in O3 abundances, primarily because photodissociation rates are drastically reduced by dust absorption. Furthermore, annual, latitudinal and seasonal cycles in dust opacity cause variations of 50% or greater in the corresponding cycles in O3 abundances. The reflectance spectroscopy technique that has been used to measure the O3 abundance may have difficulty detecting these variations.

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