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首页> 外文期刊>Geoscience and Remote Sensing, IEEE Transactions on >Bistatic Vector 3-D Scattering From Layered Rough Surfaces Using Stabilized Extended Boundary Condition Method
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Bistatic Vector 3-D Scattering From Layered Rough Surfaces Using Stabilized Extended Boundary Condition Method

机译:使用稳定扩展边界条件方法从分层粗糙表面进行双基地矢量3-D散射

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摘要

A model of 3-D electromagnetic scattering from multiple rough surfaces within homogeneous-layered or vertically inhomogeneous media is developed in this work. This model, aimed at radar remote sensing of surface-to-depth profiles of soil moisture, computes total bistatic radar cross sections from the multilayer structure based on the scattering matrix approach, cascading the scattering matrices of individual rough interfaces and the layer propagation matrices. We have recently developed the single-surface scattering matrix obtained using the stabilized extended boundary condition method (SEBCM) providing both large validity range over the surface roughness and higher computational efficiency compared to fully numerical solutions. In the presence of a vertical dielectric profile, the aggregate scattering matrix of the profile is obtained from the model of stratified homogeneous layers. Results of this multilayer SEBCM model are validated with small perturbation method of up to third order and the method of moments. Additionally, the model is used to perform a sensitivity analysis of the scattering cross section with respect to perturbations in ground parameters such as subsurface layer separation, roughness of surface and subsurface layers, and moisture content of subsurface layers. The multilayer SEBCM model developed in this work presents a realistic and computationally feasible method for solving scattering from multilayer rough surfaces of realistic roughness, providing an accurate and efficient tool for future retrievals of soil moisture profiles.
机译:在这项工作中,开发了从均质层或垂直非均质介质中的多个粗糙表面进行的3-D电磁散射模型。该模型旨在通过雷达遥感遥感土壤水分的深度到深度剖面,基于散射矩阵方法,从多层结构计算总的双基地雷达横截面,并将各个粗糙界面的散射矩阵与层传播矩阵进行级联。最近,我们开发了使用稳定扩展边界条件方法(SEBCM)获得的单表面散射矩阵,与全数值解决方案相比,该矩阵在表面粗糙度上具有较大的有效范围,并且具有较高的计算效率。在存在垂直介电轮廓的情况下,该轮廓的聚集散射矩阵是从分层的均质层模型中获得的。该多层SEBCM模型的结果已通过高达三阶的小扰动方法和矩量法得到了验证。此外,该模型还用于对散射截面相对于地面参数的扰动进行敏感性分析,例如地下层分离,表面和地下层的粗糙度以及地下层的水分含量。在这项工作中开发的多层SEBCM模型提供了一种现实可行且计算上可行的方法,用于解决从具有实际粗糙度的多层粗糙表面散射的问题,为将来获取土壤水分剖面提供了准确而有效的工具。

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