The viscous overstability, nonlinear wavetrains, and finescale structure in dense planetary rings
Abstract
This paper addresses the fine-scale axisymmetric structure exhibited in Saturn's A and B-rings. We aim to explain both the periodic microstructure on 150-220m, revealed by the Cassini UVIS and RSS instruments, and the irregular variations in brightness on 1-10km, reported by the Cassini ISS. We propose that the former structures correspond to the peaks and troughs of the nonlinear wavetrains that form naturally in a viscously overstable disk. The latter variations on longer scales may correspond to modulations and defects in the wavetrains' amplitudes and wavelength. We explore these ideas using a simple hydrodynamical model which captures the correct qualitative behaviour of a disk of inelastically colliding particles, while also permitting us to make progress with analytic and semi-analytic techniques. Specifically, we calculate a family of travelling nonlinear density waves and determine their stability properties. Detailed numerical simulations that confirm our basic results will appear in a following paper.
Cite
@article{arxiv.0904.0143,
title = {The viscous overstability, nonlinear wavetrains, and finescale structure in dense planetary rings},
author = {Henrik N. Latter and Gordon I. Ogilvie},
journal= {arXiv preprint arXiv:0904.0143},
year = {2015}
}
Comments
52 pages, 8 figures. Accepted in Icarus