The space environment of Mercury at the times of the second and third MESSENGER flybys

被引:24
作者
Baker, Daniel N. [1 ]
Odstrcil, Dusan [2 ,3 ]
Anderson, Brian J. [4 ]
Arge, C. Nick [5 ]
Benna, Mehdi [6 ]
Gloeckler, George [7 ]
Korth, Haje [4 ]
Mayer, Leslie R. [8 ]
Raines, Jim M. [7 ]
Schriver, David [9 ]
Slavin, James A. [3 ]
Solomon, Sean C. [10 ]
Travnicek, Pavel M. [9 ,11 ,12 ]
Zurbuchen, Thomas H. [7 ]
机构
[1] Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO 80303 USA
[2] George Mason Univ, Fairfax, VA 22030 USA
[3] NASA, Heliophys Sci Div, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[4] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[5] USAF, Res Lab, Kirtland AFB, NM 87117 USA
[6] NASA, Solar Syst Explorat Div, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[7] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
[8] NOAA, Boulder, CO 80303 USA
[9] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
[10] Carnegie Inst Sci, Dept Terr Magnetism, Washington, DC 20015 USA
[11] ASCR, Astron Inst, Prague 14131, Czech Republic
[12] ASCR, Inst Atmospher Phys, Prague 14131, Czech Republic
基金
美国国家科学基金会;
关键词
Mercury; Solar wind; Interplanetary magnetic field; Magnetospheres; MESSENGER; MAGNETIC-FIELD; SOLAR-WIND; 1ST FLYBY; MAGNETOSPHERE; MODEL;
D O I
10.1016/j.pss.2011.01.018
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The second and third flybys of Mercury by the MESSENGER spacecraft occurred, respectively, on 6 October 2008 and on 29 September 2009. In order to provide contextual information about the solar wind properties and the interplanetary magnetic field (IMF) near the planet at those times, we have used an empirical modeling technique combined with a numerical physics-based solar wind model. The Wang-Sheeley-Arge (WSA) method uses solar photospheric magnetic field observations (from Earth-based instruments) in order to estimate the inner heliospheric radial flow speed and radial magnetic field out to 21.5 solar radii from the Sun. This information is then used as input to the global numerical magnetohydrodynamic model, ENLIL, which calculates solar wind velocity, density, temperature, and magnetic field strength and polarity throughout the inner heliosphere. WSA-ENLIL calculations are presented for the several-week period encompassing the second and third flybys. This information, in conjunction with available MESSENGER data, aid in understanding the Mercury flyby observations and provide a basis for global magnetospheric modeling. We find that during both flybys, the solar wind conditions were very quiescent and would have provided only modest dynamic driving forces for Mercury's magnetospheric system. (C) 2011 Elsevier Ltd. All rights reserved.
引用
收藏
页码:2066 / 2074
页数:9
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