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The sand seas of Titan: Cassini RADAR observations of longitudinal dunes
Authors:Lorenz R D  Wall S  Radebaugh J  Boubin G  Reffet E  Janssen M  Stofan E  Lopes R  Kirk R  Elachi C  Lunine J  Mitchell K  Paganelli F  Soderblom L  Wood C  Wye L  Zebker H  Anderson Y  Ostro S  Allison M  Boehmer R  Callahan P  Encrenaz P  Ori G G  Francescetti G  Gim Y  Hamilton G  Hensley S  Johnson W  Kelleher K  Muhleman D  Picardi G  Posa F  Roth L  Seu R  Shaffer S  Stiles B  Vetrella S  Flamini E  West R
Institution:Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA. rlorenz@lpl.arizona.edu
Abstract:The most recent Cassini RADAR images of Titan show widespread regions (up to 1500 kilometers by 200 kilometers) of near-parallel radar-dark linear features that appear to be seas of longitudinal dunes similar to those seen in the Namib desert on Earth. The Ku-band (2.17-centimeter wavelength) images show approximately 100-meter ridges consistent with duneforms and reveal flow interactions with underlying hills. The distribution and orientation of the dunes support a model of fluctuating surface winds of approximately 0.5 meter per second resulting from the combination of an eastward flow with a variable tidal wind. The existence of dunes also requires geological processes that create sand-sized (100- to 300-micrometer) particulates and a lack of persistent equatorial surface liquids to act as sand traps.
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