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Winske & Omidi 1995
Winske, D. and Omidi, N. (1995). Diffusion at the magnetopause: Hybrid simulations. Journal of Geophysical Research 100: doi: 10.1029/94JA02730. issn: 0148-0227.

Electromagnetic wave generation and resulting cross-field diffusion of plasma are considered at a tangential discontinuity, which characterizes the magnetopause for northward interplanetary magnetic field. Two-dimensional hybrid (particle ions, massless fluid electrons) simulations, in which the tangential discontinuity is generated self-consistently via a stream-stream interaction, are used to show that wave growth occurs when the ambient magnetic field is predominantly perpendicular to the direction of the density gradient. Low-frequency (≪ion gyrofrequency) waves, with amplitudes ΔB/B≤0.2 and anticorrelated density fluctuations Δn/n≤0.6, are generated at the discontinuity, resulting in cross-field diffusion that is comparable to the Bohm rate. Both the fluctuation level and the lack of ion heating in the calculations are consistent with observations at the magnetopause. The magnitude of the diffusion is considered in the presence of numerical effects and in the context of the inferred diffusion rate at the magnetopause. The relation of the low-frequency waves and their consequences to faster growing, short-wavelength waves due to the lower hybrid drift instability is also addressed. The overall conclusion of this initial study is that diffusion due to low frequency waves is not likely to be a major effect at the magnetopause. ¿ American Geophysical Union 1995

BACKGROUND DATA FILES

Abstract

Keywords
Magnetospheric Physics, Magnetopause, cusp, and boundary layers, Space Plasma Physics, Numerical simulation studies, Space Plasma Physics, Wave/particle interactions, Space Plasma Physics, Transport processes
Journal
Journal of Geophysical Research
http://www.agu.org/journals/jb/
Publisher
American Geophysical Union
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