Anomalous ion mixing within an MHD scale Kelvin-Helmholtz vortex. 2: Effects of inhomogeneity

Details Anomalous ion mixing within an MHD scale Kelvin-Helmholtz vortex. 2: Effects of inhomogeneity Anomalous ion mixing within an MHD scale Kelvin-Helmholtz vortex. 2: Effects of inhomogeneity

Jul 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995jgr...10012025f&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 100, no. A7, p. 12,025-12,033

Physics

Geophysics

24

Geophysics, Inhomogeneity, Ions, Kelvin-Helmholtz Instability, Magnetopause, Mixing, Simulation, Vortices, Magnetohydrodynamic Stability, Mixing Layers (Fluids), Mixing Length Flow Theory, Nonuniform Magnetic Fields, Shear Layers

Scientific paper

Hybrid code simulations of the MHD scale Kelvin-Helmholtz (K-H) instability have been conducted. In contrast to the homogeneous background case where the large-scale ion mixing across the shear layer occurs inside the vortex obeying the hydrodynamic similarity law, the ion mixing is found to be reduced when the background magnetic field is inhomogeneous. This stabilization effect is twofold: it is an ion kinetic effect which reduces the saturation vortex size and so the mixing length when the shear layer width and the wavelength of the growing mode are small. The reduction effect still works even when the shear layer width/wavelength are large and a well defined vortical motion as in the fluid model is evident. The mixing is suppressed for this case because the ions on the lower magnetic field (magnetosheath) side cannot enter within the vortex island: The rolled-up magnetopause current sheet block them out electrostatically. The geophysical implication of the present result is that the K-H mixing alone may not be as efficient as to produce the large-scale mixing blob of the low-latitude boundary layer (LLBL) when the magnetic field intensity is highly different across the magnetopause.

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