Physics
Scientific paper
Apr 1990
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990georl..17..583m&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 17, April 1990, p. 583-586.
Physics
168
Current Sheets, Field Aligned Currents, Geomagnetic Tail, Magnetic Storms, Polar Substorms, Energetic Particles, International Sun Earth Explorers, Ion Currents, Magnetic Flux
Scientific paper
Throughout most of the growth phase of a substorm, the cross-tail current at x about -10 Re can be supplied by the curvature drift of a bi-directional field aligned distribution of 1 keV electrons. Just prior to its local disruption after substorm onset, the cross-tail current in the now thin (about 400 km) current sheet is carried by the cross-tail serpentine motion of non-adiabatic ions (Speiser, 1965). The instability of this latter current leads to the local disruption of the near-earth current sheet.
Frank Louis A.
Huang Chang-Yin
Mitchell Donald G.
Russell Christopher T.
Williams Jimmy D.
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