Resonance locking in giant planets indicated by the rapid orbital expansion of Titan
Val\'ery Lainey, Luis Gomez Casajus, Jim Fuller, Marco Zannoni, Paolo, Tortora, Nicholas Cooper, Carl Murray, Dario Modenini, Ryan S. Park, Vincent, Robert, Qingfeng Zhang

TL;DR
This study measures Titan's rapid orbital expansion, supporting a resonance locking tidal theory that suggests significant outward migration and revised evolutionary history for Saturn's moon system, with implications for other celestial systems.
Contribution
It provides the first direct measurements of Titan's orbital expansion rate, confirming resonance locking as a key tidal dissipation mechanism in giant planets.
Findings
Titan's orbital expansion rate is 11.3 ± 2.0 cm/year.
Resonance locking explains the observed migration and tidal dissipation.
Implications for the evolution of Saturn's moon system and other celestial systems.
Abstract
Tidal effects in planetary systems are the main driver in the orbital migration of natural satellites. They result from physical processes occurring deep inside celestial bodies, whose effects are rarely observable from surface imaging. For giant planet systems, the tidal migration rate is determined by poorly understood dissipative processes in the planet, and standard theories suggest an orbital expansion rate inversely proportional to the power 11/2 in distance, implying little migration for outer moons such as Saturn's largest moon, Titan. Here, we use two independent measurements obtained with the Cassini spacecraft to measure Titan's orbital expansion rate. We find Titan migrates away from Saturn at 11.3 2.0 cm/year, corresponding to a tidal quality factor of Saturn of Q 100, and a migration timescale of roughly 10 Gyr. This rapid orbital expansion suggests Titan…
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