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Communication Dans Un Congrès Année : 2014

The bathymetry of a Titan sea

Résumé

construct the depth profile--the bathymetry--of Titan's large sea Ligeia Mare from Cassini RADAR data collected during the 23 May 2013 (T91) nadir-looking altimetry flyby. We find the greatest depth to be about 160 m and a seabed slope that is gentler toward the northern shore, consistent with previously imaged shoreline morphologies. Low radio signal attenuation through the sea demonstrates that the liquid, for which we determine a loss tangent of 3 ± 1*10-5, is remarkably transparent, requiring a nearly pure methane-ethane composition, and further that microwave absorbing hydrocarbons, nitriles, and suspended particles be limited to less than the order of 0.1% of the liquid volume. Presence of nitrogen in the ethane-methane sea, expected based on its solubility and dominance in the atmosphere, is consistent with the low attenuation, but that of substantial dissolved polar species or suspended scatterers is not.
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Dates et versions

hal-00992841 , version 1 (19-05-2014)

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  • HAL Id : hal-00992841 , version 1

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Marco Mastrogiuseppe, Valerio Poggiali, Alexander Hayes, Ralph Lorenz, Jonathan Lunine, et al.. The bathymetry of a Titan sea. EGU, Vienna, april 2014, 2014, Vienna, Austria. ⟨hal-00992841⟩

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