Strong Localized Pumping of Water Vapor to High Altitudes on Mars During the Perihelion Season
dc.contributor.author | Brines, A. | |
dc.contributor.author | López-Valverde, M.A. | |
dc.contributor.author | Funke, B. | |
dc.contributor.author | González-Galindo, F. | |
dc.contributor.author | Aoki, S. | |
dc.contributor.author | Villanueva, G.L. | |
dc.contributor.author | Holmes, J.A. | |
dc.contributor.author | Belyaev, D.A. | |
dc.contributor.author | Liuzzi, G. | |
dc.contributor.author | Thomas, I.R. | |
dc.contributor.author | Erwin, J.T. | |
dc.contributor.author | Grabowski, U. | |
dc.contributor.author | Forget, F. | |
dc.contributor.author | Lopez-Moreno, J.J. | |
dc.contributor.author | Rodriguez-Gomez, J. | |
dc.contributor.author | Daerden, F. | |
dc.contributor.author | Trompet, L. | |
dc.contributor.author | Ristic, B. | |
dc.contributor.author | Patel, M.R. | |
dc.contributor.author | Bellucci, G. | |
dc.contributor.author | Vandaele, A.C. | |
dc.date | 2024 | |
dc.date.accessioned | 2024-07-22T09:47:08Z | |
dc.date.available | 2024-07-22T09:47:08Z | |
dc.identifier.uri | https://orfeo.belnet.be/handle/internal/13375 | |
dc.description | Here we present water vapor vertical profiles observed with the ExoMars Trace Gas Orbiter/Nadir and Occultation for MArs Discovery instrument during the perihelion and Southern summer solstice season (LS = 240°–300°) in three consecutive Martian Years 34, 35, and 36. We show the detailed latitudinal distribution of H2O at tangent altitudes from 10 to 120 km, revealing a vertical plume at 60°S–50°S injecting H2O upward, reaching abundance of about 50 ppmv at 100 km. We have observed this event repeatedly in the three Martian years analyzed, appearing at LS = 260°–280° and showing inter-annual variations in the magnitude and timing due to long term effects of the Martian Year 34 Global Dust Storm. We provide a rough estimate of projected hydrogen escape of 3.2 × 109 cm−2 s−1 associated to these plumes, adding further evidence of the key role played by the perihelion season in the long term evolution of the planet's climate. | |
dc.language | eng | |
dc.title | Strong Localized Pumping of Water Vapor to High Altitudes on Mars During the Perihelion Season | |
dc.type | Article | |
dc.subject.frascati | Physical sciences | |
dc.audience | Scientific | |
dc.subject.free | Mars | |
dc.subject.free | atmosphere | |
dc.subject.free | water vapor | |
dc.subject.free | ExoMars/TGO | |
dc.subject.free | NOMAD | |
dc.subject.free | solar occultation | |
dc.source.title | Geophysical Research Letters | |
dc.source.volume | 51 | |
dc.source.issue | 14 | |
dc.source.page | e2023GL107224 | |
Orfeo.peerreviewed | Yes | |
dc.identifier.doi | 10.1029/2023GL107224 | |
dc.identifier.url |