Saturn Ring Seismology: Looking Beyond First Order Resonances
arXiv:1402.1415 · doi:10.1016/j.icarus.2014.02.002
Abstract
Some wave features found in the C-ring of Saturn appear to be excited by resonances with normal mode oscillations of the planet. The waves are found at locations in the rings where the ratio of orbital to oscillation frequencies is given by m : m+1 where m is a small integer. I suggest here that it is plausible that ring waves may also be launched at second order resonances, where the frequency ratio would be m : m+2. Indeed, otherwise unassociated wave features are found at such locations in the C-ring. If confirmed the association of planetary modes with additional C-ring wave features would measure additional oscillation frequencies of Saturn and improve the utility of the waves for constraining the internal structure of the planet. Second-order resonances in general do not lie near first order ring resonance locations and thus are not the explanation for the apparent frequency splitting of modes.
16 pages, 2 figures. Accepted as a Note by Icarus
References in corpus (1)
Cited by in corpus (7)
- Saturn Ring Seismology: Evidence for Stable Stratification in the Deep Interior of Saturn
- Cassini Ring Seismology as a Probe of Saturn's Interior I: Rigid Rotation
- More Kronoseismology with Saturn's rings
- Kronoseismology IV. Six previously unidentified waves in Saturn's middle C ring
- The dynamics of rings around Centaurs and Trans-Neptunian Objects
- Modeling Saturn's D68 clumps as a co-orbital satellite system
- Rapid falling of an orbiting moon to its parent planet due to tidal-seismic resonance