The role of methane in Titan's clouds, climate, winds, and spin

Physics

Scientific paper

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0343 Planetary Atmospheres (5210, 5405, 5704), 5210 Planetary Atmospheres, Clouds, And Hazes (0343), 5405 Atmospheres (0343, 1060), 6281 Titan

Scientific paper

The atmosphere of Titan is laden with methane vapor, the equivalent of a 5 m global ocean. Methane is near its triple point at surface conditions on Titan, suggesting it is thermodynamically active. I will demonstrate how the coupling of methane thermodynamics to the large-scale circulation limits cloud coverage and duration, defines climate zones, limits low-altitude atmospheric superrotation, and damps the seasonal cycle. Cassini-Huygens and ground-based observations reveal these effects in the seasonality of methane clouds, the latitudinal distribution of surface morphologies, the vertical profile of winds, and a time lag in the observed seasonal spin rate change, respectively. These phenomena are consistent with the presence of an active but seasonal cycle of methane in the atmosphere.

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