Put , , and . From the exterior transform, the inverse integral has the amplitudemultiplying . Apply the supplied method of steepest descent formula at . On the outgoing sheet, , so . The far-field scattered potential isRestore for the physical time-harmonic potential. This is cylindrical outgoing spreading, with angular directivity determined by the kernel factor and aperture. The ordinary saddle formula applies for a fixed non-grazing direction, away from a coalescing pole or branch point. Its finite upstream angular limit is consistent with the separate branch-point calculation in the root solution; at grazing directions that separate calculation supplies the appropriate justification.
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