On the oscillations in Mercury's obliquity
E. Bois, N. Rambaux

TL;DR
This study models Mercury's obliquity oscillations using a spin-orbit N-body approach, revealing larger oscillation amplitudes in a full planetary interaction context, aligning with recent observations.
Contribution
Introduces a novel method to find Mercury's libration center, enabling more accurate modeling of its obliquity oscillations considering planetary interactions.
Findings
Oscillation amplitude is ten times larger in N-body case than in 2-body case.
Mean obliquity differs by about 10.8 arcseconds between models.
Results agree with recent radar observations.
Abstract
One major objective of MESSENGER and BepiColombo spatial missions is to accurately measure Mercury's rotation and its obliquity in order to obtain constraints on internal structure of the planet. Which is the obliquity's dynamical behavior deriving from a complete spin-orbit motion of Mercury simultaneously integrated with planetary interactions? We have used our SONYR model integrating the spin-orbit N-body problem applied to the solar System (Sun and planets). For lack of current accurate observations or ephemerides of Mercury's rotation, and therefore for lack of valid initial conditions for a numerical integration, we have built an original method for finding the libration center of the spin-orbit system and, as a consequence, for avoiding arbitrary amplitudes in librations of the spin-orbit motion as well as in Mercury's obliquity. The method has been carried out in two cases: (1)…
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