Neptune's Atmospheric Composition from AKARI Infrared Spectroscopy
arXiv:1003.5571 · doi:10.1051/0004-6361/200913358
Abstract
Aims: Disk-averaged infrared spectra of Neptune between 1.8 and 13 m, obtained by the AKARI Infrared Camera (IRC) in May 2007, have been analysed to (a) determine the globally-averaged stratospheric temperature structure; (b) derive the abundances of stratospheric hydrocarbons; and (c) detect fluorescent emission from CO at 4.7 m. Methods: Mid-infrared spectra were modelled using a line-by-line radiative transfer code to determine the temperature structure between 1-1000 bar and the abundances of CH, CHD and higher-order hydrocarbons. A full non-LTE radiative model was then used to determine the best fitting CO profile to reproduce the fluorescent emission observed at 4.7 m in the NG channel (with a spectral resolution of 135). Results: The globally-averaged stratospheric temperature structure is quasi-isothermal between 1-1000 bar, which suggests little variation in global stratospheric conditions since studies by the Infrared Space Observatory a decade earlier. The derived CH mole fraction of at 50 mbar, decreasing to at 1 bar, is larger than that expected if the tropopause at 56 K acts as an efficient cold trap, but consistent with the hypothesis that CH leaking through the warm south polar tropopause (62-66 K) is globally redistributed by stratospheric motion. The ratio of D/H in CH of supports the conclusion that Neptune is enriched in deuterium relative to the other giant planets. We determine a mole fraction of ethane of at 0.3 mbar, consistent with previous studies, and a mole fraction of ethylene of at 2.8 bar. An emission peak at 4.7 m is interpreted as a fluorescent emission of CO, and requires a vertical distribution with both external and internal sources of CO.
In press, accepted manuscript
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