Moist convection and the vertical structure and water abundance of Jupiter's atmosphere

Computer Science

Scientific paper

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Atmospheric Moisture, Convection Clouds, Jupiter Atmosphere, Water, Abundance, Atmospheric General Circulation Models, Cumulus Clouds, Parameterization, Thermodynamics, Jupiter, Convection, Structure, Water, Abundance, Atmosphere, Models, Circulation, Humidity, Clouds, Depletion, Water Vapor, Temperature, Depth, Thermodynamics, Diagrams, Parameters, Calculations, Plumes, Stability

Scientific paper

The cumulative effects of an ensemble of moist convective plumes on a conditionally unstable atmosphere are predicted by a model of moist convection on Jupiter in which the heating/cooling and drying/moistening of the environment occur through (1) compensating subsidence, (2) detrainment of updraft air at cloud tops, and (3) the evaporation and melting of falling condensate. Parahydrogen is transported as a passive tracer. Pure moist convective, mixed moist-dry convective, and primarily dry convective regimes are possible, depending on the assumed deep-water abundance, efficiency of condensate evaporation, and initial temperature profile.

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