Climatology of the CO vertical distribution on Mars based on ACS TGO measurements

Carbon monoxide is a non-condensable gas in the Martian atmosphere produced by the photolysis of CO2. Its abundance responds to the condensation and sublimation of CO2 from the polar caps, resulting in seasonal variations of the CO mixing ratio. ACS onboard the ExoMars Trace Gas Orbiter have measure...

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Главные авторы: Fedorova, A, Trokhimovskiy, A, Lefèvre, F, Olsen, KS, Korablev, O, Montmessin, F, Ignatiev, N, Lomakin, A, Forget, F, Belyaev, D, Alday, J, Luginin, M, Smith, M, Patrakeev, A, Shakun, A, Grigoriev, A
Формат: Journal article
Язык:English
Опубликовано: American Geophysical Union 2022

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