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    Formation of layers of methane in the atmosphere of Mars after surface release

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    Authors
    Viscardy, S.
    Daerden, F.
    Neary, L.
    Discipline
    Earth and related Environmental sciences
    Subject
    Earth atmosphere
    Orbits
    General circulation model
    Global circulation
    Mars
    Methane on Mars
    Surface emissions
    Trace gas
    Vertical distributions
    Vertical profile
    Methane
    Audience
    Scientific
    Date
    2016
    Metadata
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    Description
    Simulations with a general circulation model for the atmosphere of Mars show that surface emissions of methane can result in a highly nonuniform vertical distribution throughout the atmosphere, including the formation of layers, during the first weeks after the release. The fate of the released methane is determined by the global circulation pattern at the time of the release, and the methane can be transported to locations over the planet that are remote from the emission site. It typically takes several weeks for the methane to become more uniformly mixed, implying that the detection of vertical layers of methane can be indicative of recent surface emission. This puts the existing observations in a new perspective and will allow instruments on the upcoming ExoMars Trace Gas Orbiter mission to detect signatures of surface emission activity as they are designed to measure the first vertical profiles of methane on Mars. © 2016. American Geophysical Union. All Rights Reserved.
    Citation
    Viscardy, S.; Daerden, F.; Neary, L. (2016). Formation of layers of methane in the atmosphere of Mars after surface release. , Geophysical Research Letters, Vol. 43, Issue 5, 1868-1875, DOI: 10.1002/2015GL067443.
    Identifiers
    uri: https://orfeo.belnet.be/handle/internal/3220
    doi: http://dx.doi.org/10.1002/2015GL067443
    scopus: 2-s2.0-84960868860
    Type
    Article
    Peer-Review
    Yes
    Language
    eng
    Links
    NewsHelpdeskBELSPO OA Policy

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