Upper atmosphere temperature structure at the Venusian terminators: A comparison of SOIR and VTGCM results

被引:22
作者
Bougher, S. W. [1 ]
Brecht, A. S. [2 ,3 ]
Schulte, R. [4 ]
Fischer, J. [5 ]
Parkinson, C. D. [1 ]
Mahieux, A. [6 ,7 ]
Wilquet, V. [6 ]
Vandaele, A. [6 ]
机构
[1] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
[2] Bay Area Environm Res Inst, Sonoma, CA 95476 USA
[3] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
[4] Santa Clara Univ, Santa Clara, CA 95053 USA
[5] Univ Penn, Philadelphia, PA 19104 USA
[6] Belgian Inst Space Aeron, Planetary Aeron, Brussels, Belgium
[7] Fonds Natl Rech Sci, B-1000 Brussels, Belgium
关键词
Venus; Venus Express mission; Upper atmosphere; Thermal structure; VTGCM; Thermal balance; NEUTRAL GAS-COMPOSITION; GENERAL-CIRCULATION; GLOBAL CIRCULATION; VERTICAL STRUCTURE; PHYSICAL PROCESSES; MIDDLE ATMOSPHERE; ATOMIC OXYGEN; UPPER HAZE; THERMOSPHERE; MESOSPHERE;
D O I
10.1016/j.pss.2015.01.012
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Venus Express SOIR terminator profiles of CO2 densities and corresponding temperatures have been determined for 132 selected orbits obtained between 2006 and 2013. These recently recalibrated measurements provide temperature profiles at the Venusian terminator over approximately 70-160 km, revealing a striking permanent temperature minimum (at about 125 km) and a weaker temperature maximum (over 100-110 km). In addition, topside temperatures (above 140 km) reveal a warming trend consistent with a typical thermospheric structure. These features are reflected in the corresponding CO2 density profiles, and provide detailed constraints for global circulation models of the upper atmosphere. New Venus Thermospheric General Circulation Model (VTGCM) simulations are presented for conditions appropriate to these SOIR measurements. In particular, solar minimum to moderate fluxes are specified and mean values of eddy diffusion and wave drag parameters are utilized. Recent upgrades to the VTGCM code now include more realistic lower boundary conditions at 70 km near cloud tops. Model temperature profiles are extracted from the terminators that correspond to five latitude bins presently used in the SOIR data analysis. Averaging of VTGCM temperature profiles in each of these bins (at each terminator) is conducted to match SOIR sampling. Comparisons of these SOIR and VTGCM temperature profiles are shown. Most notably, the observed temperature minimum near 125 km and the weaker temperature maximum over 100-110 km are generally reproduced by the VTGCM at the correct pressure/altitude levels. However, magnitudes of simulated and measured temperatures are somewhat different as a function of latitude. In addition, VTGCM evening terminator (ET) temperatures are simulated to be modestly warmer than corresponding morning terminator (MT) values, a result of stronger ET than MT zonal winds at/above about 130 km. The SOIR terminator temperatures thus far do not reveal this consistent trend, suggesting the VTGCM climate based winds may not precisely represent the averaged conditions during SOIR sampling. Overall, these data-model comparisons reveal that both radiative and dynamical processes are responsible for maintaining averaged temperatures and driving significant variations in terminator temperature profiles. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:336 / 346
页数:11
相关论文
共 58 条
[31]   A new method for determining the transfer function of an Acousto optical tunable filter [J].
Mahieux, A. ;
Wilquet, V. ;
Drummond, R. ;
Belyaev, D. ;
Federova, A. ;
Vandaele, A. C. .
OPTICS EXPRESS, 2009, 17 (03) :2005-2014
[32]   In-flight performance and calibration of SPICAV SOIR onboard Venus express [J].
Mahieux, Arnaud ;
Berkenbosch, Sophie ;
Clairquin, Roland ;
Fussen, Didier ;
Mateshvili, Nina ;
Neefs, Eddy ;
Nevejans, Dennis ;
Ristic, Bojan ;
Vandaele, Ann Carine ;
Wilquet, Valerie ;
Belyaev, Denis ;
Fedorova, Anna ;
Korablev, Oleg ;
Villard, Eric ;
Montmessin, Franck ;
Bertaux, Jean-Loup .
APPLIED OPTICS, 2008, 47 (13) :2252-2265
[33]   Investigation of air temperature on the nightside of Venus derived from VIRTIS-H on board Venus-Express [J].
Migliorini, A. ;
Grassi, D. ;
Montabone, L. ;
Lebonnois, S. ;
Drossart, P. ;
Piccioni, G. .
ICARUS, 2012, 217 (02) :640-647
[34]  
Mills FP, 2007, GEOPHYS MONOGR SER, V176, P73, DOI 10.1029/176GM06
[35]   Compact high-resolution spaceborne echelle grating spectrometer with acousto-optical tunable filter based order sorting for the infrared domain from 2.2 to 4.3 μm [J].
Nevejans, Dennis ;
Neefs, Eddy ;
Van Ransbeeck, Emiel ;
Berkenbosch, Sophie ;
Clairquin, Roland ;
De Vos, Lieve ;
Moelans, Wouter ;
Glorieux, Stijn ;
Baeke, Ann ;
Korablev, Oleg ;
Vinogradov, Imant ;
Kalinnikov, Yuri ;
Bach, Benny ;
Dubois, Jean-Pierre ;
Villard, Eric .
APPLIED OPTICS, 2006, 45 (21) :5191-5206
[36]   Mass spectrometric measurements of the neutral gas composition of the thermosphere and exosphere of Venus [J].
Niemann, H. B. ;
Kasprzak, W. T. ;
Hedin, A. E. ;
Hunten, D. M. ;
Spencer, N. W. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1980, 85 (A13) :7817-7827
[37]   VENUS UPPER-ATMOSPHERE NEUTRAL GAS-COMPOSITION - 1ST OBSERVATIONS OF THE DIURNAL-VARIATIONS [J].
NIEMANN, HB ;
HARTLE, RE ;
HEDIN, AE ;
KASPRZAK, WT ;
SPENCER, NW ;
HUNTEN, DM ;
CARIGNAN, GR .
SCIENCE, 1979, 205 (4401) :54-56
[38]   Distribution of sulphuric acid aerosols in the clouds and upper haze of Venus using Venus Express VAST and VeRa temperature profiles [J].
Parkinson, Christopher D. ;
Gao, Peter ;
Schulte, Rick ;
Bougher, Stephen W. ;
Yung, Yuk L. ;
Bardeen, Charles G. ;
Wilquet, Valerie ;
Vandaele, Ann Carine ;
Mahieux, Arnaud ;
Tellmann, Silvia ;
Paetzold, Martin .
PLANETARY AND SPACE SCIENCE, 2015, 113 :205-218
[39]  
Piccialli A., 2013, VEN EXPR EUR PLAN SC, V8, P750
[40]  
Rodgers C.D., 2000, WORLD SCIENTIFIC