Magnetotail equilibrium theory - The general three-dimensional solution

Details Magnetotail equilibrium theory - The general three-dimensional solution Magnetotail equilibrium theory - The general three-dimensional solution

Oct 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987jgr....9211101b&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 92, Oct. 1, 1987, p. 11101-11108. DOE-NASA-supported research.

Physics

56

Equilibrium Equations, Geomagnetic Tail, Geomagnetism, Magnetostatics, Three Dimensional Motion, Bow Waves, Differential Equations, Earth Magnetosphere, Maxwell Equation

Scientific paper

The general magnetostatic equilibrium problem for the geomagnetic tail is reduced to the solution of ordinary differential equations and ordinary integrals. The theory allows the integration of the self-consistent magnetotail equilibrium field from the knowledge of four functions of two space variables: the neutral sheet location, the total pressure, the magnetic field strength, and the z component of the magnetic field at the neutral sheet.

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