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Atmospheric processes affecting methane on Mars

Grenfell, J. L. ; Wunderlich, F.; Sinnhuber, M. ORCID iD icon 1; Herbst, K.; Lehmann, R.; Scheucher, M.; Gebauer, S.; Arnold, G.; Rauer, H.
1 Institut für Meteorologie und Klimaforschung – Atmosphärische Spurenstoffe und Fernerkundung (IMK-ASF), Karlsruher Institut für Technologie (KIT)

Abstract:

It is currently uncertain as to whether methane exists on Mars. Data from the Curiosity Rover suggests a background methane concentration of a few tenths parts per billion whereas data from the Trace Gas Orbiter suggest an upper limit of twenty parts per trillion. If methane exists on Mars then we do not understand fully the physical and chemical processes affecting its lifetime. Atmospheric models suggest an over-estimate in the lifetime by a factor of around six hundred compared with earlier observations. In the present work we assume the Curiosity Rover background methane value and estimate the uncertainty in atmospheric chemistry and mixing processes in our atmospheric column model 1D TERRA. Results suggest that these processes can only explain a factor of ~sixteen lowering in the methane lifetime. This implies that if methane is present then additional, currently unknown processes are required to explain the observed lifetime.


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Originalveröffentlichung
DOI: 10.1016/j.icarus.2022.114940
Scopus
Zitationen: 4
Dimensions
Zitationen: 4
Zugehörige Institution(en) am KIT Institut für Meteorologie und Klimaforschung – Atmosphärische Spurenstoffe und Fernerkundung (IMK-ASF)
Publikationstyp Zeitschriftenaufsatz
Publikationsmonat/-jahr 08.2022
Sprache Englisch
Identifikator ISSN: 0019-1035
KITopen-ID: 1000148059
HGF-Programm 12.11.28 (POF IV, LK 01) The role of the near-Earth space
Erschienen in Icarus
Verlag Academic Press
Band 382
Seiten 114940
Projektinformation SPP 1992; INCREASE (DFG, DFG KOORD, SI 1088/9-1)
Vorab online veröffentlicht am 03.06.2022
Schlagwörter Mars, Atmosphere, Methane Lifetime, Photochemical, Cosmic rays
Nachgewiesen in Scopus
Web of Science
Dimensions
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