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Martian mesospheric cloud observations by IUVS on MAVEN: Thermal tides coupled to the upper atmosphere

Authors :
Gregory M. Holsclaw
A. I. F. Stewart
Franck Montmessin
William E. McClintock
M. S. Chaffin
Franck Lefèvre
D. E. Siskind
Matteo Crismani
Sonal Jain
Bruce M. Jakosky
Justin Deighan
Arnaud Stiepen
Nicholas M. Schneider
Michael H. Stevens
Daniel Lo
John Clarke
J. S. Evans
Space Science Division [Washington]
Naval Research Laboratory (NRL)
Computational Physics, Inc.
Laboratory for Atmospheric and Space Physics [Boulder] (LASP)
University of Colorado [Boulder]
Space Sciences, Technologies and Astrophysics Research Institute (STAR)
Université de Liège
Laboratoire de Physique Atmosphérique et Planétaire (LPAP)
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)
Lunar and Planetary Laboratory [Tucson] (LPL)
University of Arizona
Center for Space Physics [Boston] (CSP)
Boston University [Boston] (BU)
Source :
Geophysical Research Letters, Geophysical Research Letters, American Geophysical Union, 2017, 44 (10), pp.4709-4715. ⟨10.1002/2017GL072717⟩
Publication Year :
2017
Publisher :
American Geophysical Union (AGU), 2017.

Abstract

International audience; We report observations of Martian mesospheric ice clouds and thermospheric scale heights by the Imaging Ultraviolet Spectrograph on NASA's Mars Atmosphere and Volatile Evolution mission. The clouds are observed between 6 AM and 8 AM local time using mid-UV limb observations between 60 and 80 km tangent altitude where ice particles that scatter sunlight can appear as detached layers near the equator. The equatorial longitudinal distribution shows populations of clouds near -110° E and -10° E as well as a population near 90° E, which does not have a clear precedent. The cloud populations indicate a wave 3 pattern near 70 km, which is confirmed by independent mesospheric temperature observations. Scale heights 100 km above the clouds derived from concurrent IUVS observations also reveal a wave 3 longitudinal structure, suggesting that the temperature oscillations enabling the formation of mesospheric clouds couple to the upper atmosphere.

Details

ISSN :
19448007 and 00948276
Volume :
44
Database :
OpenAIRE
Journal :
Geophysical Research Letters
Accession number :
edsair.doi.dedup.....18505ed97feb23364f65b14f0a4b375c
Full Text :
https://doi.org/10.1002/2017gl072717