Analytical investigation of the ionospheric-plasmaspheric transfer of H(+) ions

Physics

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Continuity Equation, Hydrogen Ions, Ion Motion, Ionospheric Ion Density, Plasmasphere, Boundary Conditions, Boundary Value Problems, Diurnal Variations, Ionospheric Temperature

Scientific paper

A self-consistent description of dynamic processes in the midlatitude ionosphere and plasmasphere is obtained on the basis of an analytical solution of the equations of continuity and motion. Analytical expressions are obtained for the flux of H(+) ions from the ionosphere into the plasmasphere and back. These flux values can be used as upper boundary conditions in hybrid ionosphere models. It is shown that the diurnal-variation amplitude of H(+) concentration at the tube apex increases with increasing latitude.

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