Loss of MHD equilibrium caused by the enhancement of the magnetic By component in earth's magnetotail

Astronomy and Astrophysics – Astrophysics

Scientific paper

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Geomagnetic Tail, Magnetic Field Configurations, Magnetohydrodynamic Stability, Current Sheets, Flux Density, Magnetic Storms, Neutral Sheets

Scientific paper

A 2D MHD equilibrium theory is used to show that an enhancement of the magnetic By component in the earth's magnetotail might lead to the disruption of the near-earth cross-tail currents and thus to the onset of a magnetospheric substorm. Using numerical solutions to the linear Grad-Shafranov equation, the effect of a cross-tail magnetic field component By on MHD equilibria is illustrated. Computing sequences of quasi-static equilibria by increasing either By or the thermal plasma pressure, it is shown that the magnetosphere can change from a 'dipolar' tail structure to a tail configuration with highly sheared and/or stretched field lines. Increasing By beyond critical values may lead to catastrophic configurations in the near-earth plasma sheet, beyond which no acceptable equilibrium solution exists.

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