Effect of field-aligned potential drop in a global magnetosphere-ionosphere coupling model

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Ionospheric Currents, Magnetosphere-Ionosphere Coupling, Plasma Potentials, Volt-Ampere Characteristics, Contours, Convection, Field Aligned Currents, Solar Wind, Steady State, Voltage Generators, Vorticity

Scientific paper

Effects of field-aligned potential drops on the magnetosphere-ionosphere coupling in a steady state are studied on a global ionospheric scale. It is shown that a constant-current generator can support a larger field-aligned potential drop than a constant voltage generator under similar conditions. The magnetospheric convection pattern is distorted more in the constant current generator case than in the constant voltage generator case. The main difference between a constant current generator and a constant voltage generator is found to lie in their ability to adjust the vorticity of the magnetospheric convection. The results show that a constant current generator allows the vorticity of the magnetospheric convection to adjust so that the field-aligned current can be kept constant under the loading influence of the field-aligned potential. On the other hand, a constant voltage generator by definition cannot adjust the vorticity of the magnetospheric convection to maintain the field-aligned current under the loading influence of the field-aligned potential.

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