Polar cap arcs and their relationship to IMF and geomagnetic activity
スポンサーリンク
概要
- 論文の詳細を見る
From four months DMSP auroral image data, various kinds of polar cap arcs are examined and they may be categorized fundamentally four typical polar cap arcs. The first one is the bright arcs which occur during strong northward IMF period. The second one is poleward leap arcs which occur during the recovery phase of a substorm. The third one is multiple faint arcs which occur during the strong northward IMF period and the fourth one is very faint sun-aligned arcs which occur during a magnetically quiet period. The first and the second polar cap arcs may be originated from the plasma sheet particles. On the other hand, the third and the fourth arcs may not be related to plasma sheet particles but magnetosheath particles. Although the first and the third arcs are seen during the period of a strong northward IMF, the magnitude of geomagnetic activity for the first one is larger than that for the third one. It seems that magnetospheric energy release may be also another important factor for the auroral dynamics.
著者
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Akasofu Syun-ichi
Geophysical Institute University Of Alaska
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Makita Kazuo
Faculty Of Engineering Takusyoku University
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Makita Kazuo
Faculty Of Technology Takushoku University
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Meng Ching-i.
Applied Physics Laboratory Johns Hopkins University
関連論文
- Effects of the interplanetary magnetic field on the characteristics of Pc 3-4 pulsations at globally coordinated stations
- Occurrence conditions for two different kinds of transpolar arcs
- Polar cap arcs and their relationship to IMF and geomagnetic activity
- The polar caps
- Coordinated observations of ionosphere-atmosphere coupling in the arctic using an HF Doppler system and an infrasonic wave detector
- Polar cusp electron during quiet and disturbed period