Titan's latitudinal temperature distribution and seasonal cycle

Physics

Scientific paper

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Annual Variations, Brightness Temperature, Satellite Atmospheres, Titan, Atmospheric Composition, Methane, Nitrogen, Temperature Distribution, Voyager 1 Spacecraft, Saturn, Satellites, Titan, Latitude, Temperature, Distribution, Cycles, Seasonal Variations, Voyager 1, Iris, Infrared Interferometer Spectrometer, Brightness, Wavelengths, Troposphere, Symmetry, Models, Hydrocarbons, Polar Regions, Atmosphere, Methane, Nitrogen, Gases

Scientific paper

Voyager IRIS brightness temperature measurements of Titan at a wavelength of 530/cm are crudely indicative of ground or lower tropospheric temperatures and indicate 93 K for the equator and 91 K for both northern and southern high latitudes. The symmetry between north and south is unexpected for the time of Voyager encounter (Northern Titan spring). It is shown that this near-symmetry can arise naturally in a model where the poles are 'pinned' year-round at the dew point of CH4-N2 lakes or, more probably, a CH4-N2 rich surface layer on a deep ethane-rich ocean. For a polar temperature of 91 K, the model implies that the atmosphere contains somewhat less than 8 percent mole fraction of CH4.

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