Dynamics of the four-day circulation in the Venus atmosphere

Mathematics – Logic

Scientific paper

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Atmospheric Circulation, Dynamic Models, Eddy Viscosity, Venus Atmosphere, Angular Momentum, Atmospheric Heating, Gas Flow, Pioneer Venus Spacecraft, Planetary Rotation, Temperature Distribution, Velocity Distribution

Scientific paper

A simple axisymmetric model is constructed in order to make clear the problem of four-day circulation for the Venus atmosphere. This model incorporates the mechanisms of upward transport of angular momentum by meridional circulation, with the aid of a very large horizontal velocity that dissipates differential rotation, first proposed by Gierasch in 1975. A suppressing effect on this mechanism due to horizontal eddy viscosity finiteness is also involved. Velocity and temperature fields are represented by a few fundamental modes, and terms expressing nonlinear interactions among the modes are explicitly written in the mode equations. Stationary solutions of this system are obtained mainly by a two-layer model for both finite and infinite eddy viscosities. Results of the numerical experiments by Young and Pollack in 1977 are discussed in light of the present results.

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