Heat transfer by a meridional circulation cell and the static stability of the atmosphere of a slowly rotating planet.

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Venus Atmosphere

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Equations are derived for the determination of the equatorial-polar temperature difference and the static stability parameter in the atmosphere of a planet for which the principal heat transfer mechanism is ordered meridional circulation. The spherical geometry of the planetary atmosphere is taken into account, and the flow in the cell is specified in general form, in contrast to the a priori approximation by Stone, who was first to apply such an approach. The obtained results are investigated to evaluate the periods of thermal adaptation of the atmosphere, the scale of the wind velocity, and other characteristics of atmospheric circulation on Venus.

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