The solution of electric fields and currents in a height-resolved ionosphere is traditionally solved as an elliptic equation with Dirichlet or Neumann boundary condition in which the magnetosphere is represented as an unresponsive (prescribed) voltage generator or current source. In this paper we derive an alternative boundary condition based upon Alfvén waves in which only the Alfvén wave from the magnetosphere that is incident upon the ionosphere (Exi) is prescribed. For a uniform magnetosphere the new boundary condition reduces to ∂φ/∂z=(∂2φ/ ∂x2+2∂Exi/∂x)/(μ0VAσ≥)and is evaluated at the magnetosphere-ionosphere interface. The resulting solution is interpreted as a responsive magnetosphere and establishes a key stage in the full self-consistent and nonlinear coupling of the magnetosphere and ionosphere. Key Points An Alfvénic boundary condition for magnetosphere-ionosphere coupling is given Coupling is self-consistent and nonlinear, and ionosphere is resolved in altitude Numerical solutions are presented to demonstrate the boundary condition ©2014. American Geophysical Union. All Rights Reserved.
CITATION STYLE
Wright, A. N., & Russell, A. J. B. (2014). Alfvén wave boundary condition for responsive magnetosphere- ionosphere coupling. Journal of Geophysical Research: Space Physics, 119(5), 3996–4009. https://doi.org/10.1002/2014JA019763
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