The vertical distribution of Mars water vapor

Physics

Scientific paper

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Atmospheric Moisture, Mars Atmosphere, Vertical Distribution, Water Vapor, Air Masses, Atmospheric Models, Diurnal Variations, Mars Surface, Viking Orbiter 1, Mars, Water Vapor, Viking 1 Orbiter, Landing Sites, Viking 1, Models, Atmosphere, Scattering, Diurnal Variations, Earth-Based Observations, Water, Surface, Martian, Seasons, Annual Variations, Experiments, Dust

Scientific paper

Analysis of observations made from the Viking 1 Orbiter indicates that the water vapor over the Viking 1 landing site is uniformly mixed with the atmosphere and not concentrated near the surface. The analysis incorporates the effects of atmospheric scattering and explains why previous earth-based observations showed a strong diurnal variation in water content. It also explains the lack of an early morning fog and removes the necessity of daily exchange of large amounts of water between the surface and the atmosphere. A water vapor volume mixing ratio of 1.5 x 10 to the -4th is inferred for the Viking 1 site in late summer.

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