| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1774363 | Icarus | 2011 | 5 Pages |
Estimates of the moments of inertia of Titan, as separately deduced from its gravitational field and spin pole orientation, are quite different. This discrepancy can be resolved if Titan is either not precessing as a rigid body (e.g. if the shell is decoupled from the interior by an ocean), or if the spin pole is not fully damped (e.g. due to atmospheric excitation). By the end of the Cassini mission, continued monitoring of the changing spin pole orientation, by Cassini radar observations, will determine which effect dominates.
► For Titan, moments of inertia can be estimated from hydrostatic gravity, or from damped spin pole orientation. ► The resulting estimates are quite different. ► We suggest that the precessional estimate reflects a decoupled shell.
