The Warped Plane of the Classical Kuiper Belt
Eugene Chiang, Hyomin Choi

TL;DR
This study models the warped midplane of the Classical Kuiper Belt over four billion years, showing it precesses with a 1.9 Myr period and deviates from the invariable plane, with implications for understanding solar system dynamics.
Contribution
It provides a detailed numerical and theoretical analysis of the Kuiper Belt's warped plane, including its precession and deviation from the invariable plane, based on long-term orbital integrations.
Findings
The Kuiper belt plane precesses with a 1.9 Myr period.
The plane deviates from the invariable plane by up to a few degrees.
Current observations are consistent with planetary influence alone.
Abstract
By numerically integrating the orbits of the giant planets and of test particles over a period of four billion years, we follow the evolution of the location of the midplane of the Kuiper belt. The Classical Kuiper belt conforms to a warped sheet that precesses with a 1.9 Myr period. The present-day location of the Kuiper belt plane can be computed using linear secular perturbation theory: the local normal to the plane is given by the theory's forced inclination vector, which is specific to every semimajor axis. The Kuiper belt plane does not coincide with the invariable plane, but deviates from it by up to a few degrees in stable zones. For example, at a semimajor axis of 38 AU, the local Kuiper belt plane has an inclination of 1.9 deg and a longitude of ascending node of 149.9 deg when referred to the mean ecliptic and equinox of J2000. At a semimajor axis of 43 AU, the local plane…
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