Kronoseismology: Using density waves in Saturn's C ring to probe the planet's interior
M. M. Hedman, P. D. Nicholson

TL;DR
This study uses Cassini data to analyze density waves in Saturn's C ring, revealing patterns likely caused by Saturn's internal oscillations, offering new insights into the planet's interior structure.
Contribution
It introduces a novel method to identify and analyze density waves in Saturn's rings caused by planetary oscillations, not moons, providing constraints on Saturn's internal modes.
Findings
Six unidentified waves have 2-4 arms and specific pattern speeds.
Pattern speeds are too high for moon resonances, indicating planetary origin.
Multiple waves suggest the presence of internal planetary oscillation modes.
Abstract
Saturn's C ring contains multiple spiral patterns that appear to be density waves driven by periodic gravitational perturbations. In other parts of Saturn's rings, such waves are generated by Lindblad resonances with Saturn's various moons, but most of the wave-like C-ring features are not situated near any strong resonance with any known moon. Using stellar occultation data obtained by the Visual and Infrared Mapping Spectrometer (VIMS) onboard the Cassini spacecraft, we investigate the origin of six unidentified C-ring waves located between 80,900 and 87,200 km from Saturn's center. By measuring differences in the waves' phases among the different occultations, we are able to determine both the number of arms in each spiral pattern and the speeds at which these patterns rotate around the planet. We find that all six of these waves have between 2 and 4 arms and pattern speeds between…
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