Mercury's magnetospheric magnetic field after the first two MESSENGER flybys

被引:103
作者
Alexeev, Igor I. [1 ]
Belenkaya, Elena S. [1 ]
Slavin, James A. [2 ]
Korth, Haje [3 ]
Anderson, Brian J. [3 ]
Baker, Daniel N. [4 ]
Boardsen, Scott A. [2 ]
Johnson, Catherine L. [5 ,6 ]
Purucker, Michael E. [2 ]
Sarantos, Menelaos [2 ]
Solomon, Sean C.
机构
[1] Moscow MV Lomonosov State Univ, Scobeltsyn Inst Nucl Phys, Moscow 119992, Russia
[2] NASA, Goddard Space Flight Ctr, Heliophys Sci Div, Greenbelt, MD 20771 USA
[3] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[4] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80309 USA
[5] Univ British Columbia, Dept Earth & Ocean Sci, Vancouver, BC V6T 1Z4, Canada
[6] Carnegie Inst Sci, Dept Terr Magnetism, Washington, DC 20015 USA
关键词
Mercury; Magnetospheres; Magnetic fields; ELECTRIC-FIELDS; SPACE; MODEL;
D O I
10.1016/j.icarus.2010.01.024
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The "paraboloid" model of Mercury's magnetospheric magnetic field is used to determine the best-fit magnetospheric current system and internal dipole parameters from magnetic field measurements taken during the first and second MESSENGER flybys of Mercury on 14 January and 6 October 2008 Together with magnetic field measurements taken during the Manner 10 flybys on 29 March 1974 and 16 March 1975, there exist three low-latitude traversals separated in longitude and one high-latitude encounter From our model formulation and fitting procedure a Mercury dipole moment of 196 nT R-M(3) (where R-M is Mercury's radius) was determined The dipole is offset from Mercury's center by 405 km in the northward direction The dipole inclination to Mercury's rotation axis is relatively small, similar to 4 degrees, with an eastern longitude of 193 degrees for the dipole northern pole Our model is based on the a priori assumption that the dipole position and the moment orientation and strength do not change in time The root mean square (rms) deviation between the Mariner 10 and MESSENGER magnetic field measurements and the predictions of our model for all four flybys is 10 7 nT For each magnetic field component the rms residual is similar to 6 nT or about 1 5% of the maximum measured magnetic field, similar to 400 nT This level of agreement is possible only because the magnetospheric current system parameters have been determined separately for each flyby The magnetospheric stand-off distance, the distance from the planet's center to the inner edge of the tail current sheet, the tail lobe magnetic flux, and the displacement of the tail current sheet relative to the Mercury solar-magnetospheric equatorial plane have been determined independently for each flyby The magnetic flux in the tail lobes varied from 3 8 to 5 9 MWb, the subsolar magnetopause stand-off distance from 1 28 to 1 43 R-M. and the distance to the inner edge of the current sheet from 1 23 to 1 32 R-M The differences in the current systems between the first and second MESSENGER flybys are attributed to the effects of strong magnetic reconnection driven by southward interplanetary magnetic field during the latter flyby (C) 2010 Elsevier Inc All rights reserved
引用
收藏
页码:23 / 39
页数:17
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