Atmospheric tides and the rotation of Venus. I - Tidal theory and the balance of torques

Astronomy and Astrophysics – Astronomy

Scientific paper

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Atmospheric Tides, Planetary Rotation, Venus Atmosphere, Venus Surface, Insolation, Radar Astronomy, Solar Gravitation, Torque, Zonal Flow (Meteorology), Venus, Rotation, Atmosphere, Tidal Forces, Surface, Absorption, Heating, Circulation, Crust, Spin, Gravitational Fields, Wind, Mathematical Models, Velocity, Altitude, Pressure, Stratification, Data, Temperatures, Cooling, Obliquity, Equations Of Motion, Insolation

Scientific paper

Insolation absorbed by the surface of Venus is quickly redeposited at the bottom of the atmosphere. This periodic heating causes mass to flow away from the warm afternoon side of the planet and into the cooler morning region. The Sun's gravitational field exerts a torque on this atmospheric tide tending to accelerate the retrograde zonal circulation. When this torque is transmitted to the crust, it can balance the despinning effect of tides in the body of Venus. The slow retrograde rotation of Venus may be a steady state among tides in the atmosphere, tides in the solid body, and possibly the influence of the Earth.

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