Abstract:
The equatorial ring current is the symmetrical plasmaspheric drift current of energetic plasma trapped by the geomagnetic field. Assuming that, during a geomagnetic storm, the ring can exchange energy with other regions of the magnetosphere, a second-order differential equation must be considered as its dynamical expression, and contributions other than the solely solar-wind-induced electric field must express the forced input. The decay parameters of the recovery phase of the storm must be determined considering periods with Bz(IMF) ~Bz'(IMF) ~0.
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Citas:
---------- APA ----------
Van Zele, M.A. & Schneider, O.
(1999)
. The equatorial ring current as a part of a coupled system. Studia Geophysica et Geodaetica, 43(3), 284-288.
http://dx.doi.org/10.1023/A:1023394627630---------- CHICAGO ----------
Van Zele, M.A., Schneider, O.
"The equatorial ring current as a part of a coupled system"
. Studia Geophysica et Geodaetica 43, no. 3
(1999) : 284-288.
http://dx.doi.org/10.1023/A:1023394627630---------- MLA ----------
Van Zele, M.A., Schneider, O.
"The equatorial ring current as a part of a coupled system"
. Studia Geophysica et Geodaetica, vol. 43, no. 3, 1999, pp. 284-288.
http://dx.doi.org/10.1023/A:1023394627630---------- VANCOUVER ----------
Van Zele, M.A., Schneider, O. The equatorial ring current as a part of a coupled system. Stud. Geophys. Geod. 1999;43(3):284-288.
http://dx.doi.org/10.1023/A:1023394627630