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Title: Anomalous transport by magnetohydrodynamic Kelvin-Helmholtz instabilities in the solar wind-magnetosphere interaction

Journal Article · · J. Geophys. Res.; (United States)

A magnetohydrodynamic simulation of Kelvin-Helmholtz instabilities in a compressible plasma has been performed for parallel (v/sub 0/parallelB/sub 0/) and (v/sub 0/perpendicularB/sub 0/) configurations, modeling high-latitude (or downstream flanks) and dayside low-latitude magnetospheric boundaries. In the parallel configuration, a super-Alfvenic and transsonic shear flow (with 2<4 and M/sub s/ = V/sub 0//c/sub s/ = 1, where V/sub 0/ is the total jump of the velocity across the velocity shear layer) leads to an oscillation of the velocity shear layer, which bends the initial uniform magnetic field. With a hyper-Alfvenic shear flow (M/sub A/>4), the instability develops into a more turbulent state and the initial parallel shear flow develops into small eddies, which strongly twist, compress, and hence amplify the magnetic field by a dynamo action with an amplification factor M/sub A//2. In the nonlinear stage, however large the initial Alfven Mach number M/sub A/ may be, the magnetic field, amplified and twisted by the hydromagnetic flow vortices, eventually reacts back upon the flow evolution, and the flow vortices into smaller scale structures. In the transverse configuraion, for a fast magnetosonic Mach number M/sub f/( = V/sub 0//(c/sub s//sup 2/+v/sub A//sup 2/)/sup 1/2/) greater than a critical Mach number, the instability leads to the formation of a fast shock discontinuity from an initially subfast shear flow.

Research Organization:
Institute of Geophysics and Planetary Physics, University of California, Los Angeles
OSTI ID:
7101928
Journal Information:
J. Geophys. Res.; (United States), Vol. 89:A2
Country of Publication:
United States
Language:
English