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Two-dimensional full-wave scattering from discrete random media in layered rough surfaces

机译:分层粗糙表面中离散随机介质的二维全波散射

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Modeling of electromagnetic scattering from discrete random media in layered rough surfaces finds various applications, including depth retrieval of layered snow-covered ice and remote sensing of vegetation canopy. In this paper, a coherent technique for solving scattering from discrete random media in layered rough surfaces is presented. The significance of the development of a full-wave solution to this problem stems from the fact that both co-polarized phase difference and polarized scattering coefficients can only be accurately determined using a coherent approach. Therefore, the objective of this paper is to formulate a full-wave solution for scattering from discrete random media in layered rough surfaces as well as to demonstrate the potential in the retrieval of subsurface parameters pertaining to the physical properties of rough surfaces and discrete random media using polarized scattering coefficients and co-polarized phase difference. The core of our technique lies in the use of plane wave decomposition. Plane wave solution for the scattered field due to a rough surface is obtained using extended boundary condition method (EBCM). The recursive T-matrix algorithm together with cylindrical-waves-to-plane-waves transformation matrices is employed to deal with scattering from discrete random media. Subsequently, plane wave solutions for the scattered fields due to rough surfaces and discrete random media are then cast into reflection and transmission matrices. These reflection and transmission matrices facilitate the application of scattering matrix technique which coherently accounts for electromagnetic interactions between layered rough surfaces and discrete random media. Various numerical results are examined and it is shown that the subsurface parameters may significantly impact backscattering coefficients and co-polarized phase difference even when the subsurface ground is covered by a rough layer of discrete random media.
机译:分层粗糙表面离散随机介质的电磁散射建模发现各种应用,包括深度检索分层冰雪覆盖的冰和植被覆盖覆盖的遥感。本文介绍了一种从层状粗糙表面中的离散随机介质求解散射的相干技术。全波解决问题的发展的重要性源自:只能使用相干方法精确地确定共偏振相差和极化散射系数的事实。因此,本文的目的是为分层粗糙表面中的离散随机介质分散的全波解决方案以及展示与粗糙表面和离散随机介质的物理性质有关的地下参数的潜力使用偏振散射系数和共偏振相位差。我们技术的核心在于使用平面波分解。使用延长的边界条件法(EBCM)获得引起的散射场的平面波溶液。递归T矩阵算法与圆柱形波到平面波变换矩阵一起用于处理来自离散随机介质的散射。随后,由于粗糙表面和离散随机介质而导致的散射场的平面波解,然后投入反射和传输矩阵。这些反射和传输矩阵促进了散射矩阵技术的应用,该散射矩阵技术相干地估计层状粗糙表面和离散随机介质之间的电磁相互作用。检查各种数值结果,结果表明,即使当地下地面被离散随机介质的粗糙层覆盖时,地下参数也可以显着影响反向散射系数和共偏振相位差。

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