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...
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
|
Схожие документы
-
Revealing a high water abundance in the upper mesosphere of Mars with ACS onboard TGO
по: Belyaev, DA, и др.
Опубликовано: (2021) -
A two-Martian years survey of the water vapor saturation state on Mars based on ACS NIR/TGO occultations
по: Fedorova, A, и др.
Опубликовано: (2022) -
Thermal structure of the middle and upper atmosphere of Mars From ACS/TGO CO2 spectroscopy
по: Belyaev, DA, и др.
Опубликовано: (2022) -
No detection of SO2, H2S, or OCS in the atmosphere of Mars from the first two Martian years of observations from TGO/ACS
по: Braude, AS, и др.
Опубликовано: (2022) -
First detection of ozone in the mid-infrared at Mars: implications for methane detection
по: Olsen, KS, и др.
Опубликовано: (2020)