Modeling of the Venus atmosphere with the non-hydrostatic general circulation model

Physics

Scientific paper

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Scientific paper

A fully non-hydrostatic, gas-dynamics general circulation model of the Venus atmosphere is presented. Simulations demonstrate the development of superrotation in the deep undercloud atmosphere driven by the thermal tide. Polar vortices reproduced by the model in good agreement with observations presumably result from the interaction of superrotation with subsolar-antisolar circulation near the mesopause.

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