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Dust observations at orbital altitudes surrounding Mars.
Andersson, L; Weber, T D; Malaspina, D; Crary, F; Ergun, R E; Delory, G T; Fowler, C M; Morooka, M W; McEnulty, T; Eriksson, A I; Andrews, D J; Horanyi, M; Collette, A; Yelle, R; Jakosky, B M.
Afiliación
  • Andersson L; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA. laila.andersson@lasp.colorado.edu.
  • Weber TD; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Malaspina D; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Crary F; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Ergun RE; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Delory GT; Space Science Laboratory, University of California-Berkeley, Berkeley, CA 94720, USA.
  • Fowler CM; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Morooka MW; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • McEnulty T; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Eriksson AI; Swedish Institute of Space Physics, Uppsala, Sweden.
  • Andrews DJ; Swedish Institute of Space Physics, Uppsala, Sweden.
  • Horanyi M; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Collette A; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
  • Yelle R; Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA.
  • Jakosky BM; Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA.
Science ; 350(6261): aad0398, 2015 Nov 06.
Article en En | MEDLINE | ID: mdl-26542578
Dust is common close to the martian surface, but no known process can lift appreciable concentrations of particles to altitudes above ~150 kilometers. We present observations of dust at altitudes ranging from 150 to above 1000 kilometers by the Langmuir Probe and Wave instrument on the Mars Atmosphere and Volatile Evolution spacecraft. Based on its distribution, we interpret this dust to be interplanetary in origin. A comparison with laboratory measurements indicates that the dust grain size ranges from 1 to 12 micrometers, assuming a typical grain velocity of ~18 kilometers per second. These direct observations of dust entering the martian atmosphere improve our understanding of the sources, sinks, and transport of interplanetary dust throughout the inner solar system and the associated impacts on Mars's atmosphere.

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Science Año: 2015 Tipo del documento: Article País de afiliación: Estados Unidos

Texto completo: 1 Bases de datos: MEDLINE Idioma: En Revista: Science Año: 2015 Tipo del documento: Article País de afiliación: Estados Unidos