Drift of auroral absorption observed in February 1986 with the scanning beam riometer at Syowa Station
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概要
- 論文の詳細を見る
The scanning beam riometer at Syowa Station, Antarctica (66.1°inv. lat.) detected drift of auroral absorptions during a severe geomagnetic storm in February 1986. Eastward drifts predominated in the morning sector (0600-0930 MLT) on February 8,1986,with speeds ranging from 1.0 to 3.8km/s. These drift velocities are considerably greater than those (60-700m/s) obtained under a moderately disturbed condition reported by T. KIKUCHI et al. (Ann. Geophys., 8,431,1990) while the drift direction was the same for both cases. The eastward drift takes place with a decrease in the geomagnetic H-component, with its speed being proportional to the H-component deflection from the quiettime level. It is suggested that both the absorption drift and ionospheric currents are subjected to a common earthward electric field in the magnetosphere. Therefore, the high drift velocity may indicate an intensification of the electric field in the magnetosphere.
- 国立極地研究所の論文
著者
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Yamagishi Hisao
National Institude of Polar Research
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Kikuchi Takashi
Hiraiso Solar-Terrestrial Research Center, Communications Research Laboratory
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Kikuchi Takashi
Hiraiso Solar Terrestrial Research Center Communications Research Laboratory
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