Use , inverse factor , and . Fourier transform the homogeneous Helmholtz equation givesAn upward radiating field has no incoming component from . For , take the nonnegative real root when and the positive imaginary root when . Consequently the outgoing angular spectrum isThe propagating terms go upward; the evanescent terms decay with increasing . Grazing values are understood by a radiation limit.
There is a reference-plane qualification in the question. For an arbitrary rough surface the full line need not lie in the medium: already puts it in vacuum. In that case the stated physical trace is undefined without continuation. The exact representation is obtained instead on a plane ,One can formally set , but convergence of that continued spectrum down to the rough boundary is an additional assumption. This is the reference-plane validity of a rough-surface angular spectrum. The first boxed formula is exact in an appropriate homogeneous upper half-space; it is not automatically an exact representation at every point of a completely arbitrary rough domain. Small-height perturbation theory in part (c) uses the mean plane order by order.
For a complex harmonic field use complex conjugation in its wave-field correlation: . Put and let . Direct substitution of part (a), before imposing any homogeneity, givesThis is the general answer. It need not depend only on : even a deterministic sum of two distinct outgoing plane waves has cross terms depending on the midpoint. The requested separation-only wave-field correlation therefore presumes translation-homogeneous two-point statistics.
Under that assumption define the uncentered spectrum by . Then the height propagation of an angular-spectrum correlation isEquivalently, for the spectral measure of a stationary random field , write . This version includes coherent spectral atoms and avoids squaring Dirac delta functions. The propagating spectrum is independent of height, while an evanescent contribution is multiplied by . At the formula gives the mean wave intensity.
If the brackets instead mean the spatial autocorrelation of a finite-energy deterministic field, define . Parseval's identity gives the same integral with . That finite-energy formula must not be applied unmodified to an infinite stationary field or an infinite plane wave, whose transforms require a spectral-measure convention.
Write the unit-amplitude incident plane wave as , with . The flat Dirichlet reflected field is , so the flat total field vanishes at and has derivative .
For a controlled height expansion take with fixed regular bounded shape . Taylor expansion at the moving boundary yieldsThus the first-order scattered trace is , and its transform follows by the Translation property of the Fourier transform:The first formula is the roughness correction; the second includes the zeroth-order reflection. The small-height assumption controls the Taylor expansion for a fixed profile; arbitrarily fine surface scales can require additional derivative control, not merely a small height at fixed .
If the mean roughness height is a constant , as for stationary roughness, then . Consequently the specular first-order mean reflection isIts tangential wavenumber is unchanged and its normal wavenumber is reversed relative to incidence, which is precisely specular reflection. For zero mean height the first-order mean correction is zero, but the full mean reflected field is not zero: it still contains the flat reflection.
Small height alone does not imply the statistical conclusion. For example, deterministic mean height with produces first-order mean sidebands at and is not purely specular. Constant mean is sufficient at first order; stationarity supplies it and, with suitable translation-invariant statistics, constrains higher-order coherent reflection as well.
Articles by others on the same topic
There are currently no matching articles.