Kinetic simulations of the Kelvin-Helmholtz instability
- Los Alamos National Lab., NM (United States)
Two-dimensional hybrid simulations with particle ions and fluid electrons are used to calculate the kinetic evolution of the Kelvin-Helmholtz instability for a magnetopauselike configuration. The unindirectional magnetic field is essentially transverse to the plasma flow velocity, which is the most unstable case according to linear theory and models the flow dynamics in the subsolar region of the magnetopause for northward interplanetary magnetic field. The authors recover effects analogous to those found in MHD simulations, including a mode cascade to longer wavelengths. The boundary layer consists of coherent structure and is not well described by a diffusive process. Isolated structures on the order of the ion gyroradius are formed which can cross the boundary in either direction. The authors describe how the time evolution of these structures represents transport across boundary layers, and they consider the possible connection of these entities to flux transfer events and other structure seen in the low-latitude boundary layer at the Earth`s magnetopause as well as to flux ropes commonly observed near the ionopause of Venus. They also discuss the relation of the hybrid calculations to previous MHD simulations and to observations. 58 refs., 13 figs.
- Sponsoring Organization:
- USDOE
- OSTI ID:
- 233038
- Journal Information:
- Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: A7 Vol. 98; ISSN JGREA2; ISSN 0148-0227
- Country of Publication:
- United States
- Language:
- English
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