Represent the thin layer by its wave phase jump at the exit and take the incident envelope to have amplitude one. Then . Stationarity makes the wave phase mean a constant ; it need not be zero, since the question specifies only the variance. For a normal distribution marginal, write with . If , integration by parts in the Gaussian density gives and , hence . Thus its characteristic function gives
The Fourier transform of this constant is , interpreted distributionally for the infinite plane wave. Applying the propagator from part (a),
If the wave phase has zero mean, omit . A nonunit incident amplitude simply multiplies the expression. Only the one-point Gaussian distribution is needed for this expected value; no assumption about joint Gaussian distributions at separated points is needed.
Inverse Fourier transform of the expected value gives
independent of both coordinates. Its squared modulus is the coherent scalar wave intensity , which must not be confused with the mean wave intensity.
For the latter use the stationary two-point statistics. Let be the uncentered spectral measure of a stationary random field of , normalized by
Since , its total mass is . Under free paraxial propagation each spectral component is multiplied by ; in its wave-field correlation this wave phase multiplies its complex conjugate and cancels. The stationary intensity under free paraxial propagation is consequently
Stationarity is essential to this pointwise statement: it makes the spectral covariance diagonal. Conservation of integrated power alone would not show that a particular spatial point keeps the same scalar wave intensity.
The same result follows locally from , where . Taking expectations makes independent of , so . Thus coherent scalar wave intensity and mean wave intensity are both constant in propagation, with different values. The incoherent contribution has mean . Individual realizations can show focusing and changing scalar wave intensity even though the expected value remains constant. All these propagation statements concern the free parabolic wave equation from part (a).

Articles by others on the same topic (0)

There are currently no matching articles.