The vertical structure of CO in the Martian atmosphere from the ExoMars Trace Gas Orbiter

Carbon monoxide (CO) is the main product of CO 2 photolysis in the Martian atmosphere. Production of CO is balanced by its loss reaction with OH, which recycles CO into CO 2 . CO is therefore a sensitive tracer of the OH-catalysed chemistry that contributes to the stability of CO 2 in the atmosphere...

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Veröffentlicht in:	Nature geoscience 2021-02, Vol.14 (2), p.67-71
Hauptverfasser:	Olsen, K. S., Lefèvre, F., Montmessin, F., Fedorova, A. A., Trokhimovskiy, A., Baggio, L., Korablev, O., Alday, J., Wilson, C. F., Forget, F., Belyaev, D. A., Patrakeev, A., Grigoriev, A. V., Shakun, A.
Format:	Artikel
Sprache:	eng
Schlagworte:	704/445/823 704/445/824 704/445/845 Abundance Atmospheric and Oceanic Physics Atmospheric chemistry Atmospheric circulation Atmospheric particulates Carbon dioxide Carbon dioxide atmospheric concentrations Carbon monoxide Depletion Dust storms Earth and Environmental Science Earth Sciences Earth System Sciences Geochemistry Geology Geophysics/Geodesy Geosciences, Multidisciplinary High altitude High-altitude environments Mars Mars atmosphere Mars dust Mixing ratio Oxidation Photolysis Physical Sciences Physics Polar environments Polar regions Science & Technology Sciences of the Universe Stability Storms Trace gases Tracers Transport Upper atmosphere Vertical profiles Water vapor Water vapour
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