Physics
Scientific paper
Jun 1976
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976icar...28..269h&link_type=abstract
Icarus, vol. 28, June 1976, p. 269-278.
Physics
4
Atmospheric Moisture, Mars Atmosphere, Turbulent Diffusion, Vertical Distribution, Water Vapor, Atmospheric Boundary Layer, Atmospheric Turbulence, Condensation, Diffusion Coefficient, Flow Velocity, Optical Thickness, Troposphere, Viking Mars Program
Scientific paper
Calculations are performed of the vertical distribution of water vapor and condensate in an adiabatic atmosphere on Mars taking into account turbulent diffusion and terminal velocity. The distributions are found to be substantially different when terminal velocity is included. The eddy-diffusion coefficient in the troposphere cannot be much greater than 100,000 sq cm/sec if optical depths are to be kept low enough to be consistent with observations. Processes in the boundary layer are also discussed. It is concluded that virtually all the water vapor is to be found in the lowest 6-10 km and that the lowest 2 km should have a greater concentration than the rest of that layer. Some observational tests of these ideas and conclusion can be performed by the Viking missions to Mars.
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