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首页> 外文期刊>Earth, planets and space: EPS >Low latitude Ne and Te variations at 600 km during 1 March 1982 storm from HINOTORI satellite
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Low latitude Ne and Te variations at 600 km during 1 March 1982 storm from HINOTORI satellite

机译：HINOTORI卫星在1982年3月1日的风暴中600 km处的低纬度Ne和Te变化

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摘要

This paper presents for the first time a study of HINOTORI satellite measurements of electron density and electron temperature in the topside ionosphere exclusively for magnetic storm departures. Special focus was given to the major storm of 1 March, 1982. While large enhancements in Te characterize the day time storm response, marked increases in Ne dominate the night time deviations. The night time Ne enhancements which are rather remarkable during 0000-0400 LT are also found to be accompanied by significant Te increases, by as much as 300 K. The statistical picture that emerges from the study of a large number of storms suggests significant nocturnal Te enhancements which correlate with the magnitudes of storm intensities. Ring current particles through charge exchange processes seem to be a major source of heat input to thermal electrons, though other sources may also be important.
机译：本文首次提出了专门针对磁暴离场的HINOTORI卫星测量顶电离层中电子密度和电子温度的研究。特别关注了1982年3月1日的大风暴。虽然T e 的大幅度增强是白天暴风雨响应的特征，但N e 的显着增加主导了夜间。偏差。还发现夜间N e 的增强在0000-0400 LT期间相当显着，同时伴随着T e 的显着增加，多达300K。对大量风暴的研究得出的图片表明，夜间T e 的显着增强与风暴强度有关。通过电荷交换过程产生的环流粒子似乎是输入到热电子的主要热量来源，尽管其他来源也可能很重要。

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