摘要
Measurements of relativistic electrons (500 keV to 12 MeV) within the drift loss cone during geomagnetic storms in the spring of 1994, obtained with MKL instrument aboard the low-altitude (∼500 km) polar-orbiting satellite, CORONAS-I, are reviewed. CORONAS-I satellite observed two more pronounced electron enhancements during the period studied (March-April 1994). Time profile of Dst index indicates that these events occurred after magnetic storms on March 6-8, 1994 (Dst = -109 nT) and April 2-4, 1994 (Dst = -111 nT). Both time and L shell variations of the precipitating electron fluxes over the wide L shell range of 1-9 are presented and discussed. On the average, these fluxes had a maximum value at L = 3.8-4.6 observed during the storm recovery phases.
原文 | ???core.languages.en_GB??? |
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頁(從 - 到) | 1979-1983 |
頁數 | 5 |
期刊 | Advances in Space Research |
卷 | 36 |
發行號 | 10 |
DOIs | |
出版狀態 | 已出版 - 2005 |