Let the stationary height have covariance function , with . Define the power spectrum of surface height by
For real stationary heights this spectrum is even and nonnegative. The Fourier multiplier identity in part (c) gives
Thus coherent reflection from a stationary rough surface at normal incidence is
Require the corresponding weighted spectral moment to exist. If the stationary process has a spectral measure rather than a density, the same formula uses that measure with the matching normalization.
Splitting the propagating and evanescent parts makes the effect clear:
through second order. The positive real correction reduces the magnitude of the initially negative unit coherent reflection at this order, as some reflection becomes diffuse. The evanescent part produces a coherent wave phase correction. In contrast, the first-order mean was exactly the flat reflected wave.
The height-correlation dependence of coherent reflection cannot generally be determined from alone: the quadratic term weights the whole spectrum by , while is unweighted. If the roughness varies only on scales much longer than the wavelength, so its spectrum is concentrated at , then and
This is a useful limiting formula, not the general second-order answer under only small-height assumptions. Also the mean field sampled at the moving physical boundary is through second order, from part (c), and is a different observable.

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