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Determining Titan surface topography from Cassini SAR data
Authors:Bryan W Stiles  Scott Hensley  David M Bates  Alex Hayes  Ralph D Lorenz  Philip S Callahan  William TK Johnson  Jonathan I Lunine  Michael Janssen  Richard D West  the Cassini RADAR Team
Institution:a Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, United States
b United States Geological Survey, Flagstaff, AZ 86001, United States
c Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, United States
d Department of Geological Sciences, Brigham Young University, Provo, UT 84602, United States
e Applied Physics Laboratory, Johns Hopkins University, Laurel, MD 20723, United States
f Departments of Geophysics and Electrical Engineering, Stanford University, Stanford, CA 94305, United States
g Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, United States
h Center for Educational Technologies, Wheeling Jesuit University, Wheeling, WV 26003, United States
Abstract:A technique, referred to as SARTopo, has been developed for obtaining surface height estimates with 10 km horizontal resolution and 75 m vertical resolution of the surface of Titan along each Cassini Synthetic Aperture Radar (SAR) swath. We describe the technique and present maps of the co-located data sets. A global map and regional maps of Xanadu and the northern hemisphere hydrocarbon lakes district are included in the results. A strength of the technique is that it provides topographic information co-located with SAR imagery. Having a topographic context vastly improves the interpretability of the SAR imagery and is essential for understanding Titan.SARTopo is capable of estimating surface heights for most of the SAR-imaged surface of Titan. Currently nearly 30% of the surface is within 100 km of a SARTopo height profile. Other competing techniques provide orders of magnitude less coverage.We validate the SARTopo technique through comparison with known geomorphological features such as mountain ranges and craters, and by comparison with co-located nadir altimetry, including a 3000 km strip that had been observed by SAR a month earlier. In this area, the SARTopo and nadir altimetry data sets are co-located tightly (within 5-10 km for one 500 km section), have similar resolution, and as expected agree closely in surface height. Furthermore the region contains prominent high spatial resolution topography, so it provides an excellent test of the resolution and precision of both techniques.
Keywords:Titan  Radar observations
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