1. Martian water loss to space enhanced by regional dust storms
- Author
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Ian Thomas, D. M. Kass, Oleg Korablev, J. S. Evans, N. G. Heavens, Bojan Ristic, Gregory M. Holsclaw, Giuliano Liuzzi, Kyle Connour, Giancarlo Bellucci, Sonal Jain, Ann Carine Vandaele, Manish R. Patel, A. Kleinböhl, Justin Deighan, Michael H. Stevens, Justin Erwin, William E. McClintock, Alexander Trokhimovskiy, J. J. Lopez-Moreno, Bruce M. Jakosky, Nicholas M. Schneider, Anna Fedorova, Majd Mayyasi, Daniel Lo, Frank Daerden, Shohei Aoki, J. Y. Chaufray, Matteo Crismani, Frank Montmessin, A. I. F. Stewart, Franck Lefèvre, John Clarke, Geronimo Villanueva, M. S. Chaffin, National Science Foundation (US), National Aeronautics and Space Administration (US), Belgian Science Policy Office, Agenzia Spaziale Italiana, Agence Nationale de la Recherche (France), Centre National D'Etudes Spatiales (France), European Commission, Ministerio de Economía y Competitividad (España), Ministerio de Ciencia, Innovación y Universidades (España), Laboratory for Atmospheric and Space Physics [Boulder] (LASP), University of Colorado [Boulder], Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency [Sagamihara] (JAXA), Space Research Institute of the Russian Academy of Sciences (IKI), Russian Academy of Sciences [Moscow] (RAS), Department of Atmospheric and Planetary Sciences [Hampton] (APS), Hampton University, PLANETO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS), Center for Space Physics [Boston] (CSP), Boston University [Boston] (BU), Computational Physics, Inc., Naval Research Laboratory (NRL), NASA Goddard Space Flight Center (GSFC), California State University [San Bernardino] (CSUSB), Lunar and Planetary Laboratory [Tucson] (LPL), University of Arizona, Belgian Institute for Space Aeronomy / Institut d'Aéronomie Spatiale de Belgique (BIRA-IASB), Instituto de Astrofísica de Andalucía (IAA), Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), School of Physical Sciences [Milton Keynes], Faculty of Science, Technology, Engineering and Mathematics [Milton Keynes], The Open University [Milton Keynes] (OU)-The Open University [Milton Keynes] (OU), Istituto di Astrofisica e Planetologia Spaziali - INAF (IAPS), and Istituto Nazionale di Astrofisica (INAF)
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Martian ,010504 meteorology & atmospheric sciences ,Hydrogen ,Atmospheric circulation ,animal diseases ,chemistry.chemical_element ,Astronomy and Astrophysics ,Storm ,Mars Exploration Program ,Forcing (mathematics) ,Atmospheric sciences ,01 natural sciences ,7. Clean energy ,Observational evidence ,chemistry ,13. Climate action ,[SDU]Sciences of the Universe [physics] ,0103 physical sciences ,Environmental science ,010303 astronomy & astrophysics ,0105 earth and related environmental sciences - Abstract
Full list of authors: Chaffin, M. S.; Kass, D. M.; Aoki, S.; Fedorova, A. A.; Deighan, J.; Connour, K.; Heavens, N. G.; Kleinbohl, A.; Jain, S. K.; Chaufray, J. -Y.; Mayyasi, M.; Clarke, J. T.; Stewart, A. I. F.; Evans, J. S.; Stevens, M. H.; McClintock, W. E.; Crismani, M. M. J.; Holsclaw, G. M.; Lefevre, F.; Lo, D. Y.; Montmessin, F.; Schneider, N. M.; Jakosky, B.; Villanueva, G.; Liuzzi, G.; Daerden, F.; Thomas, I. R.; Lopez-Moreno, J. -J.; Patel, M. R.; Bellucci, G.; Ristic, B.; Erwin, J. T.; Vandaele, A. C.; Trokhimovskiy, A.; Korablev, O. I., Mars has lost most of its initial water to space as atomic hydrogen and oxygen. Spacecraft measurements have determined that present-day hydrogen escape undergoes large variations with season that are inconsistent with long-standing explanations. The cause is incompletely understood, with likely contributions from seasonal changes in atmospheric circulation, dust activity and solar extreme ultraviolet input. Although some modelling and indirect observational evidence suggest that dust activity can explain the seasonal trend, no previous study has been able to unambiguously distinguish seasonal from dust-driven forcing. Here we present synoptic measurements of dust, temperature, ice, water and hydrogen on Mars during a regional dust event, demonstrating that individual dust events can boost planetary H loss by a factor of five to ten. This regional storm occurred in the declining phase of the known seasonal trend, establishing that dust forcing can override this trend to drive enhanced escape. Because similar regional storms occur in most Mars years, these storms may be responsible for a large fraction of Martian water loss and represent an important driver of Mars atmospheric evolution. © 2021, The Author(s), under exclusive licence to Springer Nature Limited., This research was supported by NASA through the MAVEN and MRO projects. IUVS data products were produced using the RMACC Summit supercomputer, which is supported by the National Science Foundation (award nos. ACI-1532235 and ACI-1532236), by the University of Colorado Boulder and by Colorado State University. The Summit supercomputer is a joint effort of the University of Colorado Boulder and Colorado State University. M.M.J.C. is supported by the NASA Postdoctoral Program at the NASA Goddard Space Flight Center, which is administered by the Universities Space Research Association under contract with NASA. A.K. acknowledges support from the NASA Mars Data Analysis Program (80NM0018F0719). Work at the Jet Propulsion Laboratory, California Institute of Technology, is performed under contract with NASA. ExoMars is a space mission of the European Space Agency and Roscosmos. The NOMAD experiment is led by the Royal Belgian Institute for Space Aeronomy (BIRA-IASB), assisted by co-principal investigator teams from Spain (IAA-CSIC), Italy (INAF-IAPS) and the United Kingdom (Open University). For this project we acknowledge funding by the Belgian Science Policy Office, with financial and contractual coordination by the European Space Agency Prodex Office (PEA 4000103401 and 4000121493); by the Spanish MICINN through its Plan Nacional; by European funds under grant nos. PGC2018-101836-B-I00 and ESP2017-87143-R (MINECO/FEDER); by the United Kingdom Space Agency through grant nos. ST/R005761/1, ST/P001262/1, ST/R001405/1 and ST/S00145X/1; and by the Italian Space Agency through grant no. 2018-2-HH.0. The IAA-CSIC team acknowledges financial support from the State Agency for Research of the Spanish MCIU through the ‘Center of Excellence Severo Ochoa’ award for the Instituto de Astrofísica de Andalucía (SEV-2017-0709). This work was supported by the Belgian Fonds de la Recherche Scientifique-FNRS under grant nos. 30442502 (ET_HOME) and T.0171.16 (CRAMIC) and by the Belgian Science Policy Office BrainBe SCOOP Project. S.A. is ‘Chargé de Recherches’ at the F.R.S.-FNRS. NOMAD’s United States investigators are supported by NASA. Science operations of ACS on TGO are funded by Roscosmos and the ESA. IKI affiliates acknowledge support from the Ministry of Science and Higher Education of the Russian Federation. F.M. acknowledges funding from the CNES and ANR (PRCI, CE31 AAPG2019-MCUBE project).
- Published
- 2021
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