Fig. 1
Geometry showing the scattering process in the atmospheric co-ordinate system (Z-axis along the atmospheric normal). The magnetic field makes an angle θB with respect to the polar Z-axis, and has an azimuth χB. (θ′,χ′) refer to the incident ray, and (θ,χ) to the scattered ray defined with respect to the polar Z-axis. Θ is the scattering angle.
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