AAS 196th Meeting, June 2000
Session 1. Planetary Rings: a Brief History of Observation and Theory
Invited, Monday, June 5, 2000, 8:30-9:20am, Lilac Ballroom

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[1.01] Planetary Rings: a Brief History of Observation and Theory

P. D. Nicholson (Cornell University)

Over several centuries, and extending down to today, the ring systems encircling Saturn and the other jovian planets have provided an endless source of speculation and theorizing for astronomers, theologians, and physicists. In the past two decades they have also become a testing ground for dynamical models of more distant astrophysical disks, such as those which surround protostars and even the stellar disks of spiral galaxies. I will review some of the early theories, and their sometimes rude confrontation with observational data, starting with Christiaan Huygens and touching on seminal contributions by Laplace, Bessel, Maxwell, Barnard, Russell (of H-R diagram fame) and Jeffreys. In the modern era, observations at infrared and radio wavelengths have revealed Saturn's rings to be composed of large chunks of almost pure water ice, and to have a vertical thickness measured in tens of meters. A renaissance in planetary rings studies occurred in the period 1977--1981, first with the discoveries of the narrow, dark and non-circular rings of Uranus and the tenuous jovian ring system, and capped off by the spectacular images returned during the twin Voyager flybys of Saturn. Along with the completely unsuspected wealth of detail these observations revealed came an unwelcome problem: are the rings ancient or are we privileged to live at a special time in history? The answer to this still-vexing question may lie in the complex gravitational interactions recent studies have revealed between the rings themselves and their retinues of attendant satellites. Between the four known ring systems, we see elegant examples of Lindblad and corotation resonances (first invoked in the galactic context), electromagnetic resonances, many-armed spiral density waves and bending waves, narrow ringlets which exhibit internal modes due to a collective instability, sharp-edged gaps maintained via tidal torques from embedded moonlets, and tenuous dust belts created by meteoroid impact onto parent bodies. I will conclude with a glimpse at what may well be a dynamicist's worst nightmare --- Saturn's multi-stranded, kinky and clumpy F ring, which continues to puzzle 20 years after it was first seen. The author would like to acknowledge many discussions with Joe Burns, Jeff Cuzzi, Luke Dones, Jim Elliot, Dick French, Peter Goldreich, Mark Showalter and Bruno Sicardy, as well as generous support from NASA.


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