Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

MHD model for the complete open magnetotail boundary

Journal Article · · J. Geophys. Res.; (United States)
In the Coroniti-Kennel MHD model for the open magnetotail boundary, a standing slow-mode expansion fan turns the magnetosheath flow into the plasma mantle and converts the magnetosheath field into the tail lobe field. The expansion fan-plasma mantle is also called the high-latitude boundary layer. The Coroniti-Kennel model applies to the noon-midnight meridian plane and the case of a purely southward interplanetary magnetic field (IMF). This paper (1) quantitatively tests and verifies the model, and (2) describes how the relatively thick and rapidly propagating high-latitude expansion fan automatically thins and slows at lower latitudes. It tapers down to a thin, nonpropagating tangential discontinuity representing the low-latitude boundary layer on closed field lines. Thus the model shows how the dawn-to-dusk current sheet that bisects the tail horizontally can return to dawn over the tail's back uninterruptedly across a seamless juncture between the high- and low-latitude boundary layers. Other important properties emerge from the complete boundary mode. A rotational discontinuity preconditions the field to pass through the slow mode wave. It induces a secondary circulation in the cross-sectional plane. This circulation sweeps plasma sheet plasma dawnward and duskward away from the tail's midplane and draws it up the tail's flanks, possibly accounting for the plasma sheet's butterfly-shaped cross section. The along-the-tail currents flowing on the rotational discontinuity have the same IMF B/sub y/ dependence as the cusp currents, which they might feed. The B/sub y/ distortion of the secondary circulation tends to rotate the plasma sheet about the tail axis to face the IMF. copyright American Geophysical Union 1987
Research Organization:
Department of Atmospheric Sciences, University of California, Los Angeles
OSTI ID:
6277550
Journal Information:
J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 92:A7; ISSN JGREA
Country of Publication:
United States
Language:
English