“…The commonly used surface height probability distribution function is the Gaussian distribution. The non-Gaussian surface height profile has been studied and generated using different approaches [15,16], and finds certain applications in practical situation. Transformation methods can be used to generate the non-Gaussian random surface [17].…”
Section: Description Of the Statistical Surfacementioning
Abstract-The electromagnetic scattering from a perfectly electric conducting (PEC) target located above or below rough surface is investigated, for the case of TM polarization, using the Method of
“…The commonly used surface height probability distribution function is the Gaussian distribution. The non-Gaussian surface height profile has been studied and generated using different approaches [15,16], and finds certain applications in practical situation. Transformation methods can be used to generate the non-Gaussian random surface [17].…”
Section: Description Of the Statistical Surfacementioning
Abstract-The electromagnetic scattering from a perfectly electric conducting (PEC) target located above or below rough surface is investigated, for the case of TM polarization, using the Method of
“…In our previous paper [7] we used the generalized experimental spectrum of surface presented in [8]. But this spectrum does not agree with the PDF of slopes based on [2] data.…”
Section: Determining the Parameters Of The Pdfmentioning
“…To approach an answer to this question we developed in [13] a statistical model of the surface that possesses the following properties: (1) It has the given PDF of elevations in any fixed point of the surface. (2) It has the given anisotropic spectrum.…”
Section: Which Statistical Characteristics Of the Surface Completely mentioning
confidence: 99%
“…PDF. The model developed in [13] is only one of many possibilities. Some related problems were considered earlier in [14][15][16][17].…”
Section: Which Statistical Characteristics Of the Surface Completely mentioning
confidence: 99%
“…Note that all of the values ∆ 1 , (27) to (29) in terms of conditional mean values (13) to (17), we obtain:…”
Section: Joint Pdf For Upwind and Cross-wind Differences In Elevationmentioning
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