Accurate free and forced rotational motions of rigid Venus

TL;DR

This paper models the precise free and forced rotational motions of Venus, including polhody and nutation, at milliarcsecond accuracy, highlighting differences from Earth's rotational behavior due to Venus's unique properties.

Contribution

It provides the first detailed computation of Venus's polhody and nutation coefficients, extending previous models with high-precision analytical and numerical methods.

Findings

Venus's polhody is highly elliptical with a 525-century period.

Nutation coefficients for Venus's third axis are comparable to Earth's.

Significant differences exist between the nutation of Venus's figure axis and angular momentum axis.

Abstract

% context :The precise and accurate modelling of a terrestrial planet like Venus is an exciting and challenging topic, all the more interesting since it can be compared with that of the Earth for which such a modelling has already been achieved at the milliarcsecond level % aims: We want to complete a previous study (Cottereau and Souchay, 2009), by determining at the milliarcsecond level the polhody, i.e. the torque-free motion of the axis of angular momentum of a rigid Venus in a body-fixed frame, as well as the nutation of its third axis of figure in space, which is fundamental from an observational point of view. results :In a first part we have computed the polhody, i.e. the respective free rotational motion of the axis of angular momentum of Venus with respect to a body-fixed frame. We have shown that this motion is highly elliptical, with a very long period of 525 cy to be compared with 430 d for the Earth. This is due to the very small dynamical flattening of Venus in comparison with our planet. In a second part we have computed precisely the Oppolzer terms which allow to represent the motion in space of the third Venus figure axis with respect to Venus angular momentum axis, under the influence of the solar gravitational torque. We have determined the corresponding tables of coefficients of nutation of the third figure axis both in longitude and in obliquity due to the Sun, which are of the same order of amplitude as for the Earth. We have shown that the coefficients of nutation for the third figure axis are significantly different from those of the angular momentum axis on the contrary of the Earth. Our analytical results have been validated by a numerical integration which revealed the indirect planetary effects.