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Resonant Alfven wave heating of the plasma sheet boundary layer

Journal Article · · Journal of Geophysical Research; (United States)
The exchange of energy between the plasma mantle and the plasma sheet boundary layer (PSBL) is examined with a one-dimensional magnetotail model. The energy exchange occurs via Poynting flux generated by the localized mode conversion of a surface wave to an Alfven wave. This Poynting flux propagates through the lobe and into the PSBL where it is absorbed by two processes. The first arises from a gradient in the plasma {beta} causing a smooth absorption of Poynting flux. The second process results from the localized mode conversion of the decaying surface wave to an Alfven wave, causing a localized absorption of energy. A numerical solution of the linearized ideal MHD equations is obtained by assuming an adiabatic equation of state. The energy flux absorbed within the PSBL is of the order of 1 {mu}W/m{sup 2} (assuming a fluid displacement of 1 R{sub E} at the plasma mantle) and varies with central plasma sheet temperature in a manner capable of triggering a thermal catastrophe in the boundary layer.
OSTI ID:
5370951
Journal Information:
Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 95:A9; ISSN 0148-0227; ISSN JGREA
Country of Publication:
United States
Language:
English