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Transverse cusp diffraction catastrophes: pertinent wavefronts and a Pearcey approximation to the wave field

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Abstract

Longitudinal cusp caustics (which unfold along the direction of propagation) are of interest when modeling the focusing produced by the passage of light through irregular media1 or reflected by curved surfaces. In the present research I model diffraction patterns characteristic of transverse cusp caustics which unfold perpendicular to the propagation direction of the most strongly focused ray. It is assumed that the amplitude exp [ik(g — ct)] in an x-y plane results from propagation (from an unfocused source) through irregularities or from reflection. If this wave is to propagate beyond the x-y plane in a homogeneous medium to produce a shear-free transverse cusp, it is sufficient to consider g = a1x2 + a2y2x + a3y2, a2 ≠ 0, with real aj. The Fresnel approximation of the resulting 2-D diffraction integral gives a wave field proportional to the 1-D Pearcy integral P(X, Y) or to P*(X, Y) depending on the sign of a1 + (2z)−1 where z is the distance beyond the x-y plane. The real parameters X, Y depend on the aj, z, k, and the transverse coordinates in the observation plane. Stationary-phase points of the diffraction integral locate the rays from the x-y plane to the observation point.

© 1986 Optical Society of America

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