Impulsive penetration and viscous interaction

摘要: How the magnetosheath plasma enters entry layer and low latitude boundary layers, with particle energy spectra almost unchanged is investigated. It was proposed by Lemaire that this accomplished impulsive penetration of clouds plasmoids. Once inside magnetosphere, a plasmoid its own momentum will polarize, to create electric field for continued motion. This voltage generator charges up sides in process creating internal magnetospheric field. The particles gradient curvature drift, constituting still another generator, current power processes. may be explanation viscous interaction first Axford Hines.