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Originally published in Science Express on 2 April 2009
Science 15 May 2009:
Vol. 324. no. 5929, pp. 921 - 923
DOI: 10.1126/science.1168905

Reports

Size and Shape of Saturn's Moon Titan

Howard A. Zebker,1,* Bryan Stiles,2 Scott Hensley,2 Ralph Lorenz,3 Randolph L. Kirk,4 Jonathan Lunine5

Cassini observations show that Saturn’s moon Titan is slightly oblate. A fourth-order spherical harmonic expansion yields north polar, south polar, and mean equatorial radii of 2574.32 ± 0.05 kilometers (km), 2574.36 ± 0.03 km, and 2574.91 ± 0.11 km, respectively; its mean radius is 2574.73 ± 0.09 km. Titan’s shape approximates a hydrostatic, synchronously rotating triaxial ellipsoid but is best fit by such a body orbiting closer to Saturn than Titan presently does. Titan’s lack of high relief implies that most—but not all—of the surface features observed with the Cassini imaging subsystem and synthetic aperture radar are uncorrelated with topography and elevation. Titan’s depressed polar radii suggest that a constant geopotential hydrocarbon table could explain the confinement of the hydrocarbon lakes to high latitudes.

1 Departments of Geophysics and Electrical Engineering, Stanford University, Stanford, CA 94305, USA.
2 Jet Propulsion Laboratory (JPL), California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
3 Applied Physics Laboratory, Johns Hopkins University, 11100 Johns Hopkins Road, Laurel, MD 20723, USA.
4 U.S. Geological Survey, 2255 North Gemini Drive, Flagstaff, AZ 86001, USA.
5 Departments of Planetary Science and Physics, University of Arizona, Tucson, AZ 85721, USA.

* To whom correspondence should be addressed. E-mail: zebker{at}stanford.edu

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