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Fig. 8


Stokes I and Q/I profiles at the surface for different values of the heliocentric angle computed for the angle-averaged (dashed lines) and the angle-dependent (solid lines) PRD. The bottom three panels show the absolute difference in Q/I between the AA and AD profiles. The atmospheric model used is (T,a,ϵ,r,ΓER) = (2 × 104,10-3,10-4,0,0).

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