Effective Conductivity of a Cloudy Ionosphere - Hydromagnetic Waves in the Magnetosphere and the Ionosphere - page 312

then

exp i ( q + p ) r =1 , if q + p =0 ,

(10. A.4)

exp i ( q + p ) r =0 , if q + p =0 .

Substituting δϕ ( q ) from (10. A.2) we have

+
q

B l ( q )

j i = σ ik e k δσ il ( − q )

q i q m

e l q l (10. A.5)

σ im

which is the basis for calculation of the effective conductivity σ eff

ik .

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