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A map of D/H on Mars in the thermal infrared using EXES aboard SOFIA

Encrenaz, T. (författare)
LESIA - Laboratoire d'Etudes Spatiales et d'Instrumentation en Astrophysique
Dewitt, C. (författare)
University of California, Davis
Richter, M. J. (författare)
University of California, Davis
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Greathouse, T. K. (författare)
Southwest Research Institute (swri), Texas
Fouchet, T. (författare)
LESIA - Laboratoire d'Etudes Spatiales et d'Instrumentation en Astrophysique
Montmessin, F. (författare)
Institute Pierre Simon Laplace
Lefèvre, F. (författare)
Institute Pierre Simon Laplace
Forget, F. (författare)
Laboratoire de Meteorologie Dynamique
Bézard, B. (författare)
LESIA - Laboratoire d'Etudes Spatiales et d'Instrumentation en Astrophysique
Atreya, S. K. (författare)
University of Michigan
Case, M. (författare)
University of California, Davis
Ryde, N. (författare)
Lund University,Lunds universitet,Astronomi - Genomgår omorganisation,Institutionen för astronomi och teoretisk fysik - Genomgår omorganisation,Naturvetenskapliga fakulteten,Lund Observatory - Undergoing reorganization,Department of Astronomy and Theoretical Physics - Undergoing reorganization,Faculty of Science
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 (creator_code:org_t)
2016-01-26
2016
Engelska.
Ingår i: Astronomy and Astrophysics. - : EDP Sciences. - 0004-6361 .- 1432-0746. ; 586
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • On a planetary scale, the D/H ratio on Mars is a key diagnostic for understanding the past history of water on the planet; locally, it can help to constrain the sources and sinks of water vapor through the monitoring of condensation and sublimation processes. To obtain simultaneous measurements of H2O and HDO lines, we have used the Echelle Cross Echelle Spectrograph (EXES) instrument aboard the Stratospheric Observatory for Infrared Astronomy (SOFIA) facility to map the abundances of these two species over the Martian disk. High-resolution spectra (R = 6 × 104) were recorded in the 1383-1390 cm-1 range (7.2 μm) on April 08, 2014. Mars was very close to opposition and near northern summer solstice (Ls = 113°). Maps of the H2O and HDO mixing ratios were retrieved from the line depth ratios of weak H2O and HDO transitions divided by a weak CO2 line. As expected for this season, the H2O and HDO maps show a distinct enhancement toward polar regions, and their mixing ratios are consistent with previous measurements and with predictions by the global climate models, except at the north pole where the EXES values are weaker. We derive a disk-integrated D/H ratio of 6.8 (+1.6, -1.0) × 10-4. It is higher than the value in Earth's oceans by a factor 4.4 (+1.0, -0.6). The D/H map also shows an enhancement from southern to northern latitudes, with values ranging from about 3.5 times to 6.0 times the VSMOW (Vienna standard mean ocean water) value. The D/H distribution shows a depletion over the Tharsis mountains and is consistent with observed latitudinal variations. The variations in D/H with latitude and altitude agree with the models and with the isotope fractionation expected from condensation and sublimation processes.

Ämnesord

NATURVETENSKAP  -- Fysik -- Astronomi, astrofysik och kosmologi (hsv//swe)
NATURAL SCIENCES  -- Physical Sciences -- Astronomy, Astrophysics and Cosmology (hsv//eng)

Nyckelord

Infrared: planetary systems
Planets and satellites: atmospheres
Planets and satellites: composition
Planets and satellites: terrestrial planets

Publikations- och innehållstyp

art (ämneskategori)
ref (ämneskategori)

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