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Boundary layer model for magnetospheric substorms. Progress report

Technical Report ·
OSTI ID:6832588
Magnetospheric-substorm activity is presently understood as the combined effect of energy transport and dissipation directly driven through the solar-terrestrial interaction and of the unloading of energy stored in the magnetotail. Many studies of particle and field signatures of substorms in the magnetotail have led to the proposal that a neutral line forms close to the Earth at the time of expansive phase onset with the plasma-sheet population on the anti-Earthward side of the neutral line ultimately being lost to the solar wind through the ejection of the plasmoid. This reprint presents an alternative framework in which substorm effects in the magnetosphere can be understood. Observations of magnetic-field and plasma-flow variations in the magnetotail can be explained in terms of the passage of the plasma sheet boundary layer over the satellite detecting the tail signatures. Field-aligned currents and particle acceleration processes on magnetic-field lines threading the ionospheric Harang discontinuity lead to the distinctive particle and field signatures observed in the magnetotail during substorms. Edge effects of field-aligned currents associated with the westward-traveling surge can lead to the negative Bz perturbations observed in the tail that are presently attributed to observations made on the anti-Earthward side of a near-Earth neutral line.
Research Organization:
Iowa Univ., Iowa City (USA). Dept. of Physics and Astronomy
OSTI ID:
6832588
Report Number(s):
AD-A-194400/8/XAB; N-00014-85-K-0404
Country of Publication:
United States
Language:
English