Journal of Geophysical Research, VOL. 99, NO. A6, PAGES 11,277-11,295, JUNE 1, 1994.
Cross-tail current, field-aligned current, and By
Richard L. Kaufmann, Chen Lu, and Douglas J. Larson
Department of Physics, University of New Hampshire, Durham
Abstract. Orbits of individual charged particles were traced in a one-dimensional magnetic field model that
included a uniform cross-tail component Byo. The effects of on the cross-tail current distribution , the
average cross-tail drift velocity , and the average pitch angle change ·DaŅ experienced during current
sheet encounters were calculated. The addition of a that exceeded several tenths of one nanotesla com-
pletely eliminated all resonance effects for odd-N orbits. An odd-N resonance involves ions that enter and exit
the current sheet on the same side. Pitch angles of nearly all such ions changed substantially during a typical
current sheet interaction, and there was no region of large cross-tail drift velocity in the presence of a modest
. The addition of a very large guide field in the direction that enhances the natural drift produces a large
jy and small ·DaŅ for ions with all energies. The addition of a modest Byo had less effect near even-N resonances.
In this case, ions in a small energy range were found to undergo so little change in pitch angle that particles
which originated in the ionosphere would pass through the current sheet and return to the conjugate ionosphere.
Finally, the cross-tail drift of ions from regions dominated by stochastic orbits to regions dominated by either
resonant or guiding center orbits was considered. The ion drift speed changed substantially during such transi-
tions. The accompanying electrons obey the guiding center equations, so electron drift is more uniform. Any
difference between gradients in the fluxes associated with electron and ion drifts requires the presence of a Bir-
keland current in order to maintain charge neutrality. This plasma sheet region therefore serves as a current gen-
erator. The analysis predicts that the resulting Birkeland current connects to the lowest altitude equatorial
regions in which ions drift to or from a point at which stochastic orbits predominate. The proposed mechanism
appears only in analyses that include non-guiding-center effects.
Paper Number 94JA00490