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Theory of imperfect magnetosphere-ionosphere coupling

Journal Article · · Geophys. Res. Lett.; (United States)
A theory of magnetosphere-ionosphere coupling in the presence of field-aligned potential drops is formulated within the framework of magnetohydrodynamic equations. Our formulation allows the magnetosphere as well as the ionosphere to respond self-consistently to the parallel potential drop along auroral field lines. Equipotential contours are distorted into a V-shaped structure near the convection reversal boundary and S-shaped on the equatorward side, each gives rise to an inverted V precipitation band. The loading effect of the imperfect coupling results in a valley in the electric field profile which occurs equatorward of the convection reversal boundary.
Research Organization:
Geophysical Institute, University of Alaska, Fairbanks, Alaska 99701
OSTI ID:
7095820
Journal Information:
Geophys. Res. Lett.; (United States), Journal Name: Geophys. Res. Lett.; (United States) Vol. 7:9; ISSN GPRLA
Country of Publication:
United States
Language:
English