Computer modeling of magnetotail convection

Physics

Scientific paper

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Geomagnetic Tail, Magnetic Field Configurations, Magnetohydrodynamic Waves, Neutral Sheets, Plasma-Electromagnetic Interaction, Electric Fields, Electromagnetic Interactions, Lorentz Force, Plasma Layers, Pressure Gradients, Time Dependence

Scientific paper

Birn and Schindler (1983) have presented a self-consistent theory of convection in the geomagnetic tail for relatively quiet times. Conditions are considered when the flow speeds are small in comparison to typical MHD wave speeds, and a quasi-static approximation neglecting inertia terms in the equation of motion is valid. In the present investigation, a time-dependent nonlinear ideal two-dimensional MHD code is used to study the response of the magnetotail to an externally applied dawn-to-dusk electric field Ev. It is found that for Ev approximately equal to or less than 1 mV/m the quasi-static approximation is generally a good approximation as long as no tail instabilities are generated. Assuming that the near-earth boundary is essentially closed to particle losses, it is found that the magnetotail changed in time consistent with changes which are believed to characterize the substorm growth phase.

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