Interplanetary and magnetospheric electr
β
Y. Kamide
π
Article
π
2001
π
Elsevier Science
π
English
β 188 KB
Most of the Dst variance during intense geomagnetic storms can be reproduced by changes in large-scale electric ΓΏelds in the solar wind. Whether successive substorms (in other words, magnetospheric electric ΓΏelds) play a direct role in the energization of storm-time ring current particles is the sub