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Probing the Martian atmosphere with MAVEN/IUVS stellar occultations

Authors :
William E. McClintock
Nicholas M. Schneider
S. W. Bougher
Matteo Crismani
Gaetan Lacombe
Justin Deighan
Michael Chaffin
A. I. F. Stewart
Roger V. Yelle
Arnaud Stiepen
Paul R. Mahaffy
Gregory M. Holsclaw
Hannes Gröller
Franck Montmessin
Sonal Jain
Bruce M. Jakosky
John Clarke
Franck Lefèvre
Tommi Koskinen
Lunar and Planetary Laboratory [Tucson] (LPL)
University of Arizona
PLANETO - LATMOS
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Laboratory for Atmospheric and Space Physics [Boulder] (LASP)
University of Colorado [Boulder]
Center for Space Physics [Boston] (CSP)
Boston University [Boston] (BU)
NASA Goddard Space Flight Center (GSFC)
Department of Atmospheric, Oceanic, and Space Sciences [Ann Arbor] (AOSS)
University of Michigan [Ann Arbor]
University of Michigan System-University of Michigan System
Source :
Geophysical Research Letters, Geophysical Research Letters, American Geophysical Union, 2015, 42 (21), pp.9064-9070. ⟨10.1002/2015GL065294⟩, Geophysical Research Letters, 2015, 42 (21), pp.9064-9070. ⟨10.1002/2015GL065294⟩
Publication Year :
2015
Publisher :
HAL CCSD, 2015.

Abstract

International audience; The first campaign of stellar occultations with the Imaging Ultraviolet Spectrograph (IUVS) instrument on board of Mars Atmosphere and Volatile EvolutioN (MAVEN) mission was executed between 24 and 26 March 2015. From this campaign 13 occultations are used to retrieve CO2 and O2 number densities in the altitude range between 100 and 150 km. Observations probe primarily the low-latitude regions on the nightside of the planet, just past the dawn and dusk terminator. Calculation of temperature from the CO2 density profiles reveals that the lower thermosphere is significantly cooler than predicted by the models in the Mars Climate Database. A systematically cold layer with temperatures of 105–120 K is seen in the occultations at a pressure level around 7 × 10−6 Pa.

Details

Language :
English
ISSN :
00948276 and 19448007
Database :
OpenAIRE
Journal :
Geophysical Research Letters, Geophysical Research Letters, American Geophysical Union, 2015, 42 (21), pp.9064-9070. ⟨10.1002/2015GL065294⟩, Geophysical Research Letters, 2015, 42 (21), pp.9064-9070. ⟨10.1002/2015GL065294⟩
Accession number :
edsair.doi.dedup.....e7f6c1703362e760e3a9b4114ca6bf8e
Full Text :
https://doi.org/10.1002/2015GL065294⟩