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Fig. 1

image

Geometry of the BLR models investigated. STOKES allows us to parameterize cylindrical and conical emission regions. The thin Keplerian disk geometry is obtained by taking a height that is much smaller than the outer radius rout (upper left). The polar wind geometry is a thin hollow bicone with an opening angle going from α1 = 45° to α2 = 60° (right). The equatorial wind geometry is built using the same conical geometry as for the polar wind but with α1 = 75° and α2 = 90°, resulting in a flared disk with an opening angle of 30° (lower left).

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