Continuous tailward flow in the near-Earth magnetotail observed by TC-1 satellite

被引:0
|
作者
Zhang, LingQian [1 ]
Liu, ZhenXing
Ma, ZhiWei
Pu, ZuYin
Wang, JiYe
Shen, Chao
机构
[1] Chinese Acad Sci, Ctr Space Sci & Appl Res, Beijing 100080, Peoples R China
[2] Chinese Acad Sci, Inst Plasma Phys, Hefei 230031, Peoples R China
[3] Peking Univ, Sch Earth & Space Sci, Beijing 100871, Peoples R China
[4] Natl Cent Univ, Phys & Electron Engn Acad, Beijing 100081, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2007年 / 52卷 / 14期
基金
中国国家自然科学基金;
关键词
substorm onset; dipolarization; southward IMF; tailward flow;
D O I
10.1007/s11434-007-0228-7
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
On July 11, 2004, a substorm process in the period of continuous tailward flow was observed by the joint exploration of the TC-1, IMAGE and ACE satellites. The substorm observed by the TC-1 in the near-Earth has three stages: the growth phase (from 11:43 to 12:19), the pre-expansion process (from 12:19 to 12:28) and the dipolarization process. The auroral brightening was at 12:26 recorded by the FUV instrument on IMAGE, and the dipolarization occurred two minutes later. During the 45 min period of the tailward flow, the magnetotail experienced the growth phase and the pre-expansion process. When the dipolarization process began, the TC-1 entered the plasma sheet and observed a high speed earthward flow. The field-aligned tailward flow is characterized by the low temperature and high density, which is consistent with the properties of the flow from the ionosphere detected in the near-Earth magnetotail by other satellites. The tailward flow is closely related with the southward interplanetary magnetic field (IMF), and may have an important effect on the substorm.
引用
收藏
页码:1980 / 1985
页数:6
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