Two-step development of geomagnetic storms

被引:229
|
作者
Kamide, Y [1 ]
Yokoyama, N
Gonzalez, W
Tsurutani, BT
Daglis, IA
Brekke, A
Masuda, S
机构
[1] Nagoya Univ, Solar Terr Environm Lab, Toyokawa, Aichi 442, Japan
[2] Univ Tromso, Auroral Observ, N-9037 Tromso, Norway
[3] Natl Observ Athens, Inst Ionspher & Space Res, Palea Penteli 15236, Greece
[4] Inst Nacl Pesquisas Espaciais, BR-12200 Sao Jose Dos Campos, SP, Brazil
[5] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
关键词
D O I
10.1029/97JA03337
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Using the Dst index, more than 1200 geomagnetic storms, from weak to intense, spanning over three solar cycles have been examined statistically. Interplanetary magnetic field(IMF) and solar wind data have also been used in the study. It is found that for more than 50% of intense magnetic storms, the main phase undergoes a two-step growth in the ring current. That is, before the ring current has decayed significantly to the prestorm level, anew major particle injection occurs, leading to a further development of the ring current, and making Dst decrease a second time. Thus intense magnetic storms may often be the result of two closely spaced moderate storms. The corresponding signature in the interplanetary medium is the arrival of double-structured southward IMF at the magnetosphere.
引用
收藏
页码:6917 / 6921
页数:5
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