Alfvenic noise and transient reconfiguration in a simulated current sheet

Details Alfvenic noise and transient reconfiguration in a simulated current sheet Alfvenic noise and transient reconfiguration in a simulated current sheet

Nov 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992georl..19.2195r&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 19, no. 22, p. 2195-2198.

Physics

3

Current Sheets, Geomagnetic Tail, Magnetic Field Reconnection, Two Dimensional Models, Cyclotron Resonance, Ion Beams, Magnetohydrodynamic Waves, Particle In Cell Technique

Scientific paper

The code by Hamilton and Eastwood (1982) is used to model a magnetotail-like structure with a nonsymmetrical topology in order to develop a self-consistent steady-state model. The model is found to support the magnetic perturbations caused by cyclotron resonance interactions with features similar to ion beams. The model demonstrates field reconfiguration and particle responses similar to those in near-earth substorms when the model is subjected to transient changes in the convection electric field.

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