The response of the magnetotail to changes in the IMF orientation: The magnetotail's long memory

被引:37
作者
Walker, RJ [1 ]
Richard, RL
Ogino, T
Ashour-Abdalla, M
机构
[1] Univ Calif Los Angeles, Inst Geophys & Planetary Phys, Los Angeles, CA 90095 USA
[2] Nagoya Univ, Solar Terr Environm Lab, Aichi 442, Japan
[3] Univ Calif Los Angeles, Dept Phys, Los Angeles, CA 90095 USA
来源
PHYSICS AND CHEMISTRY OF THE EARTH PART C-SOLAR-TERRESTIAL AND PLANETARY SCIENCE | 1999年 / 24卷 / 1-3期
基金
美国国家航空航天局;
关键词
D O I
10.1016/S1464-1917(98)00032-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We have used a three dimensional global magnetohydrodynamic simulation of the interaction between the solar wind and the magnetosphere to investigate the changes which occur in the magnetotail when the interplanetary magnetic field (IMF) changes orientation. For IMF B-y not equal 0 the entire magnetotail twists when the IMF changes from southward to northward. The twisting at a given location on the tail magnetopause occurs shortly after the IMF change reaches that location. inside the magnetosphere the response time is much longer. New field lines with open ends formed by the reconnection of tail lobe field at a near-Earth neutral line also twist as the field lines convect tailward. Initially formed with a southward B-z they end up with a northward B-z. The response of the tail to a change in the IMF is controlled by the penetration of the solar wind electric field into the magnetosphere. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:221 / 227
页数:7
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