Orbital evolution of Saturn's mid-sized moons and the tidal heating of Enceladus
Ayano Nakajima, Shigeru Ida, Jun Kimura, Ramon Brasser

TL;DR
This study uses N-body simulations to explore how Saturn's mid-sized moons evolved orbitally, highlighting the role of ring torque in avoiding resonance trapping and explaining Enceladus's high heat flow through eccentricity excitation.
Contribution
It demonstrates that ring torque can prevent resonance trapping and sustain eccentricity, providing a plausible explanation for Enceladus's observed heat flow, which previous models struggled to explain.
Findings
Ring torque influences orbital evolution, avoiding resonance trapping.
Eccentricity excitation from rings can account for Enceladus's heat.
Most simulations show potential for collision, but ring mass decrease may prevent it.
Abstract
The formation and orbital evolution of Saturn's inner mid-sized moons are still debated. The most puzzling aspects are 1) how the Tethys-Dione pair and the Mimas-Enceladus pair passed through their strong 3:2 mean-motion resonances during the tidal orbital evolution, and 2) the current strong heat flow from Enceladus, which is a few orders of magnitude higher than the tidal energy dissipation caused by the present orbital eccentricity of Enceladus. Here we perform N-body simulations of the moons' orbital evolution from various initial conditions -- assuming that the moons were formed from Saturn's hypothetical massive ring -- and investigate possible paths to solve the above difficulties. If the influence of the rings is neglected, we find that the Tethys-Dione pair cannot avoid becoming trapped in the mean-motion resonances as they recede from Saturn, and that the Tethys-Enceladus pair…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
