Eddy diffusion coefficient for the atmosphere of Venus from radio scintillation measurements

Physics

Scientific paper

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Atmospheric Temperature, Diffusion Coefficient, Radio Occultation, Scintillation, Turbulent Diffusion, Venus Atmosphere, Energy Dissipation, Pioneer Venus Spacecraft, Prandtl Number, Richardson Number, Tropopause, Venus, Atmosphere, Eddy Diffusion, Coefficients, Scintillations, Dynamics, Photochemistry, Temperatures, Radio Occultations, Tropopause, Turbulence, Shear, Energy, Dissipation, Observations

Scientific paper

Estimates are obtained of the vertical mass eddy diffusion coefficient of the Venus atmosphere in the region of turbulence near 60 km on the basis of radio scintillations observed during radio occultation by the atmosphere. The structure constant estimated from Pioneer Venus orbit 18 entrance radio occultation measurements is used, under the assumption that the turbulence is generated by wind-shear, to derive a value of 40,000 sq cm/sec for the vertical mass eddy diffusion coefficient, together with an energy dissipation rate of 20 sq cm/sec and a temperature fluctuation dissipation rate of 0.001 K-squared/sec. Results are noted to fall within the range measured for the earth's troposphere, however, indicate that small-scale turbulence is probably the dominant mechanism for vertical transport near the tropopause in the Venus atmosphere.

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