M. Hesse et al., HYBRID MODELING OF THE FORMATION OF THIN CURRENT SHEETS IN MAGNETOTAIL CONFIGURATIONS, Journal of Geomagnetism and Geoelectricity, 48(5-6), 1996, pp. 749-763
Hybrid simulations are used to investigate the formation of a thin cur
rent sheet inside the plasma sheet of a magnetotail-like configuration
. The initial equilibrium is subjected to a driving electric field qua
litatively similar to what would be expected from solar wind driving.
As a result, we find the formation of a new current sheet, with a thic
kness of approximately the ion inertial length. The current density in
side the current sheet region is supplied largely by the electrons. Io
n acceleration in the cross-tail direction is absent due since the dri
ving electric field fails to penetrate into the equatorial region. The
ions in the thin current sheet region exhibit anisotropies which appe
ar to be driven by the bounce motion in the z direction between the in
ward moving plasma sheet-lobe boundary.