A study of geomagnetic storms
Substorm
Ring current
Ionospheric dynamo region
Geomagnetic secular variation
DOI:
10.1111/j.1365-246x.1978.tb05494.x
Publication Date:
2007-04-02T23:58:37Z
AUTHORS (2)
ABSTRACT
An attempt is made to find interplanetary magnetic field and solar-wind parameters which control the development of geomagnetic storms. For this purpose, energy flux estimated in terms Poynting (E×B/4π), its time variations are compared with rate dissipation ring-current particle injection ui(t), Joule ionosphere uj(t) auroral up(t) for 15 major A large increase u(t) associated substorm activity. Thus, ∈(t) entering magnetosphere dissipated through magneto-spheric processes within magnetosphere, their accumulated effects can be understood as storm phenomena.
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