Weighing Uranus' moon Cressida with the $\eta$ ring

Abstract

The $\eta$ ring is one of the narrow rings of Uranus, consisting of a dense core that is 1-2 km wide and a diffuse outer sheet spanning about 40 km. Its dense core lies just exterior to the 3:2 Inner Lindblad Resonance of the small moon Cressida. We fit the $\eta$ ring radius residuals and longitudes from a complete set of both ground-based and Voyager stellar and radio occultations of the Uranian rings spanning 1977-2002. We find variations in the radial position of the $\eta$ ring that are likely generated by this resonance, and take the form of a 3-lobed structure rotating at an angular rate equal to the mean motion of the moon Cressida. The amplitude of these radial oscillations is $0.667\pm 0.113$ km, which is consistent with the expected shape due to the perturbations from Cressida. The magnitude of these variations provides the first measurement of the mass and density of the moon Cressida ($m=2.5\pm 0.4\times 10^{17}$ kg and $\rho =0.86\pm 0.16$ g/cm${}^3$) or, indeed, any of Uranus' small inner moons. A better grasp of inner Uranian satellite masses will provide another clue to the composition, dynamical stability, and history of Uranus' tightly packed system of small moons.

Accepted for publication in AJ

References in corpus (4)

• Compositions and origins of outer planet systems: Insights from the Roche critical density
• Cupid is Doomed: An Analysis of the Stability of the Inner Uranian Satellites
• The Architecture of the Cassini Division
• Resonant Chains and Three-body Resonances in the Closely-Packed Inner Uranian Satellite System

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• Uranus' hidden narrow rings
• A Pluto--Charon Sonata IV. Improved Constraints on the Dynamical Behavior and Masses of the Small Satellites
• Cupid Is Not Doomed Yet: On the Stability of the Inner Moons of Uranus