The methane mole fraction in Titan’s stratosphere from DISR measurements during the Huygens probe’s descent

•We analyze Huygens/DISR spectra to determine the CH4 abundance in Titan’s stratosphere.•We use recently published methane linelist for the 1.4-μm band.•Derived methane mole fraction agrees with Huygens/GCMS measurement.•Result is not consistent with recent Cassini/CIRS determination at low latitude...

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Bibliographic Details
Published inIcarus (New York, N.Y. 1962) Vol. 242; pp. 64 - 73
Main Author Bezard, Bruno
Format Journal Article
LanguageEnglish
Published Elsevier Inc 01.11.2014
Elsevier
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Summary:•We analyze Huygens/DISR spectra to determine the CH4 abundance in Titan’s stratosphere.•We use recently published methane linelist for the 1.4-μm band.•Derived methane mole fraction agrees with Huygens/GCMS measurement.•Result is not consistent with recent Cassini/CIRS determination at low latitudes. We present a determination of the methane mole fraction in Titan’s stratosphere using spectral measurements by the Upward Looking Infrared Spectrometer (ULIS) of the Descent Imager/Spectral Radiometer (DISR) aboard the Huygens probe. We analyzed the 1.4-μm band of methane for which a complete linelist, down to very low intensities, was recently made available. The DISR/ULIS measurements were used to derive the methane transmittance along the path from the probe to the Sun during the descent from 135 to 29km. Fitting the transmittance ratios to remove residual instrumental effects, we derived a stratospheric methane mole fraction of 1.44 (+0.27/−0.11)%, taking into account random errors and uncertainties in the spectroscopic parameters. This value is fully consistent with the simultaneous measurement of the methane profile by the Huygens Gas Chromatograph/Mass Spectrometer (GCMS). It disagrees with the ∼1% mixing ratio recently inferred from Cassini/CIRS spectra at low latitudes near 85km. Possible reasons for the discrepancy and uncertainties in the methane spectroscopic parameters are discussed.
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ISSN:0019-1035
1090-2643
DOI:10.1016/j.icarus.2014.07.013