Article (Scientific journals)
Understanding the variability of nightside temperatures, NO UV and O2 IR nightglow emissions in the Venus upper atmosphere
Brecht, A. S.; Bougher, Stephen W.; Gérard, Jean-Claude et al.
2011In Journal of Geophysical Research. Planets, 116, p. 08004
Peer reviewed
 

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Keywords :
Planetary Sciences: Solid Surface Planets: Atmospheres (0343; 1060); Planetary Sciences: Solid Surface Planets: Aurorae and airglow; Planetary Sciences: Solid Surface Planets: Composition (1060; 3672); Planetary Sciences: Solar System Objects: Venus
Abstract :
[en] Venus Express (VEX) has been monitoring key nightglow emissions and thermal features (O[SUB]2[/SUB] IR nightglow, NO UV nightglow, and nightside temperatures) which contribute to a comprehensive understanding of the global dynamics and circulation patterns above ˜90 km. The nightglow emissions serve as effective tracers of Venus' middle and upper atmosphere global wind system due to their variable peak brightness and horizontal distributions. A statistical map has been created utilizing O[SUB]2[/SUB] IR nightglow VEX observations, and a statistical map for NO UV is being developed. A nightside warm layer near 100 km has been observed by VEX and ground-based observations. The National Center for Atmospheric Research (NCAR) Venus Thermospheric General Circulation Model (VTGCM) has been updated and revised in order to address these key VEX observations and to provide diagnostic interpretation. The VTGCM is first used to capture the statistically averaged mean state of these three key observations. This correspondence implies a weak retrograde superrotating zonal flow (RSZ) from ˜80 km to 110 km and above 110 km the emergence of modest RSZ winds approaching 60 m s[SUP]-1[/SUP] above ˜130 km. Subsequently, VTGCM sensitivity tests are performed using two tuneable parameters (the nightside eddy diffusion coefficient and the wave drag term) to examine corresponding variability within the VTGCM. These tests identified a possible mechanism for the observed noncorrelation of the O[SUB]2[/SUB] and NO emissions. The dynamical explanation requires the nightglow layers to be at least ˜15 km apart and the retrograde zonal wind to increase dramatically over 110 to 130 km.
Disciplines :
Space science, astronomy & astrophysics
Author, co-author :
Brecht, A. S.;  Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, USA) ; AB(Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, USA) ; AC(Laboratoire de Physique Atmosphérique et Planétaire, Université de Liège, Liège, Belgium) ; AD(Department of Atmospheric, Oceanic, and Space Sciences, University of Michigan, Ann Arbor, Michigan, USA) ; AE(Department of Space Studies, Southwest Research Institute, Boulder, Colorado, USA) ; AF(High Altitude Observatory, National Center for Atmospheric Research, Boulder, Colorado, USA
Bougher, Stephen W.
Gérard, Jean-Claude  ;  Université de Liège - ULiège > Département d'astrophys., géophysique et océanographie (AGO) > Labo de physique atmosphérique et planétaire (LPAP)
Parkinson, C. D.
Rafkin, S.
Foster, B.
Language :
English
Title :
Understanding the variability of nightside temperatures, NO UV and O2 IR nightglow emissions in the Venus upper atmosphere
Publication date :
01 August 2011
Journal title :
Journal of Geophysical Research. Planets
ISSN :
2169-9097
eISSN :
2169-9100
Publisher :
American Geophysical Union (AGU), Washington D.C., United States
Volume :
116
Pages :
08004
Peer reviewed :
Peer reviewed
Available on ORBi :
since 13 October 2011

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