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Kan 1993
Kan, J.R. (1993). A global magnetosphere-ionosphere coupling model of substorms. Journal of Geophysical Research 98: doi: 10.1029/93JA01168. issn: 0148-0227.

A global model of substorms is proposed on the basis of observational synthesis and theoretical modeling. Since the theoretical basis of the present model is the magnetosphere-ionosphere coupling (MIC) process, it will be called the MIC model of substorms. Substorms can occur in the MIC model without a new X line formed in the near-Earth plasma sheet, in contrast to the highly popular near-Earth neutral line (NENL) model of substorms. Following enhanced dayside reconnection, the ionosphere overloads both the solar wind on open field lines and the plasma sheet on closed field lines. The solar wind responds to the overload by providing more driven energy from the dynamo action on open field lines. The plasma sheet responds to the overload by collapsing itself, i.e., dipolarizing its field configuration to form the substorm current wedge. The explosive intensification during the expansion phase is powered by releasing the magnetic energy stored on closed field lines in the plasma sheet. The stored energy is released by the unloading instability driven by a positive feedback in the substorm current wedge. ¿ American Geophysical Union 1993

BACKGROUND DATA FILES

Abstract

Keywords
Magnetospheric Physics, Storms and substorms, Ionosphere, Ionosphere-magnetosphere interactions, Magnetospheric Physics, Current systems, Magnetospheric Physics, Auroral phenomena
Journal
Journal of Geophysical Research
http://www.agu.org/journals/jb/
Publisher
American Geophysical Union
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