The post-terminator ionosphere of Venus

被引:7
作者
Fox, Jane L. [1 ]
机构
[1] Wright State Univ, Dept Phys, Dayton, OH 45435 USA
关键词
Venus; Atmosphere; Ionospheres; Atmospheres; Chemistry; Composition; NIGHTSIDE IONOSPHERE; SOLAR-CYCLE; ELECTRON-TEMPERATURE; DAYSIDE IONOSPHERE; THERMAL STRUCTURE; EMPIRICAL-MODELS; UPPER-ATMOSPHERE; ION; DYNAMICS; DENSITY;
D O I
10.1016/j.icarus.2011.09.020
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We have modeled the near and post-terminator thermosphere/ionosphere of Venus with a view toward understanding the relative importance of EUV solar fluxes and downward fluxes of atomic ions transported from the dayside in producing the mean ionosphere. We have constructed one-dimensional thermosphere/ionosphere models for high solar activity for seven solar zenith angles (SZAs) in the dusk sector: 90 degrees, 95 degrees, 100 degrees, 105 degrees, 110 degrees, 115 degrees and 125 degrees. For the first 4 SZAs, we determine the optical depths for solar fluxes from 3 A to 1900 A by integrating the neutral densities numerically along the slant path through the atmosphere. For SZAs of 90 degrees, 95 degrees, and 100 degrees, we first model the ionospheres produced by absorption of the solar fluxes alone; for 95 degrees, 100 degrees, and 105 degrees SZAs, we then model the ion density profiles that result from both the solar source and from imposing downward fluxes of atomic ions, including O+, Ar+, C+, N+, H+, and He+, at the top of the ionospheric model in the ratios determined for the upward fluxes in a previous study of the morphology of the dayside (60 degrees SZA) Venus ionosphere. For SZAs of 110 degrees, 115 degrees and 125 degrees, which are characterized by shadow heights above about 300 km, the models include only downward fluxes of ions. The magnitudes of the downward ion fluxes are constrained by the requirement that the model O+ peak density be equal to the average O+ peak density for each SZA bin as measured by the Pioneer Venus Orbiter Ion Mass Spectrometer. We find that the 90 and 95 SZA model ionospheres are robust for the solar source alone, but the O+ peak density ill the "solar-only" 95 SZA model is somewhat smaller than the average value indicated by the data. A small downward flux of ions is therefore required to reproduce the measured average peak density of O+. We find that, on the nightside, the major ion density peaks do not occur at the altitudes of peak production, and diffusion plays a substantial role in determining the ion density profiles. The average downward atomic ion flux for the SZA range of 90-125 degrees is determined to be about 1.2 x 10(8) cm(-2) s(-1). (C) 2011 Elsevier Inc. All rights reserved.
引用
收藏
页码:625 / 639
页数:15
相关论文
共 91 条
[1]  
[Anonymous], 1967, SCIENCE, V158, P1678, DOI 10.1126/science.158.3809.1678
[2]   Evolution of the solar ionizing flux [J].
Ayres, TR .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 1997, 102 (E1) :1641-1651
[3]   The loss of ions from Venus through the plasma wake [J].
Barabash, S. ;
Fedorov, A. ;
Sauvaud, J. J. ;
Lundin, R. ;
Russell, C. T. ;
Futaana, Y. ;
Zhang, T. L. ;
Andersson, H. ;
Brinkfeldt, K. ;
Grigoriev, A. ;
Holmstrom, M. ;
Yamauchi, M. ;
Asamura, K. ;
Baumjohann, W. ;
Lammer, H. ;
Coates, A. J. ;
Kataria, D. O. ;
Linder, D. R. ;
Curtis, C. C. ;
Hsieh, K. C. ;
Sandel, B. R. ;
Grande, M. ;
Gunell, H. ;
Koskinen, H. E. J. ;
Kallio, E. ;
Riihela, P. ;
Sales, T. ;
Schmidt, W. ;
Kozyra, J. ;
Krupp, N. ;
Franz, M. ;
Woch, J. ;
Luhmann, J. ;
McKenna-Lawlor, S. ;
Mazelle, C. ;
Thocaven, J. -J. ;
Orsini, S. ;
Cerulli-Irelli, R. ;
Mura, M. ;
Milillo, M. ;
Maggi, M. ;
Roelof, E. ;
Brandt, P. ;
Szego, K. ;
Winningham, J. D. ;
Frahm, R. A. ;
Scherrer, J. ;
Sharber, J. R. ;
Wurz, P. ;
Bochsler, P. .
NATURE, 2007, 450 (7170) :650-653
[4]  
Bauer S.J., 1986, ADV SPACE RES, V11, P233
[5]  
Bauer S. J., 2004, Planetary Aeronomy: Atmosphere Environments in Planetary Systems
[6]  
Bauer S.J., 1973, PHYS PLANETARY IONOS
[7]   The dynamic behavior of the Venus ionosphere in response to solar wind interactions [J].
Brace, L. H. ;
Theis, R. F. ;
Hoegy, W. R. ;
Wolfe, J. H. ;
Mihalov, J. D. ;
Russell, C. T. ;
Elphic, R. C. ;
Nagy, A. F. .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1980, 85 (A13) :7663-7678
[8]   THE NIGHTWARD ION FLOW SCENARIO AT VENUS REVISITED [J].
BRACE, LH ;
HARTLE, RE ;
THEIS, RF .
ATMOSPHERES OF VENUS AND MARS, 1995, 16 (06) :99-112
[9]   PLASMA CLOUDS ABOVE THE IONOPAUSE OF VENUS AND THEIR IMPLICATIONS [J].
BRACE, LH ;
THEIS, RF ;
HOEGY, WR .
PLANETARY AND SPACE SCIENCE, 1982, 30 (01) :29-37
[10]   EVIDENCE FOR DAY-TO-NIGHT ION-TRANSPORT AT LOW SOLAR-ACTIVITY IN THE VENUS PRE-DAWN IONOSPHERE [J].
BRANNON, JF ;
FOX, JL ;
PORTER, HS .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (23) :2739-2742