Comments on the Venus rotation pole

Astronomy and Astrophysics – Astronomy

Scientific paper

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Astrometry, Orbit Perturbation, Planetary Rotation, Venus (Planet), Oblate Spheroids, Radar Astronomy, Solar System, Tides, Venus, Rotation, Position (Location), Spin, Obliquity, Radar, Data, Coupling, Viscosity

Scientific paper

Possible orientations of the Venus rotation pole as a function of planetary oblateness are calculated, taking into account the variation of the orbital inclination and motion of the nodal line produced by long-term planetary perturbations and assuming the obliquity to be fully damped. If the obliquity is stabilized against solar tides by core-mantle viscous coupling, a fully damped obliquity is the expected state. An analysis of earth-based radar data from 1964 to 1977 yields a pole position which lies near damped pole positions of small oblateness, no more than about 10 to the 6th. Possible implications of this result are considered.

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