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Numerical analysis of global ionospheric current system including the effect of equatorial enhancement
A modeling method is proposed to derive a two-dimensional ionospheric layer conductivity, which is appropriate to obtain a realistic solution of the polar-originating ionospheric current system including equatorial enhancement. The model can be obtained by modifying the conventional, thin shell conductivity model. It is shown that the modi®cation for one of the non-diagonal terms (S hu ) in the conductivity tensor near the equatorial region is very important; the term in¯uences the pro®le ofdoi:10.1007/s00585-999-0692-2 fatcat:bmfli27nbff6zl5doacufoilc4