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Physics-Based Modeling and Electromagnetic Scattering Computation for Snow-Packs

机译:积雪的基于物理的建模和电磁散射计算

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Physics-based Fully-Coherent Electromagnetic (EM) scattering model from 3D snowpack with arbitrary thickness is considered. The computer-generated snow media is reconstructed using the implementation of the Lineal-Path function in conjunction with 3D spatial exponential correlation function to assure the macroscopic connectivity of the snow particles. A fully-coherent EM computation is performed using the Statistical S-Matrix Wave Propagation- in Spectral domain approach (SSWaP-SD) along with a Method of Moments (MoM) code based on the Discrete-Dipole Approximation (DDA). This approach is chosen to leverage both the time-efficient computations of the DDA and the full-coherency of the SSWaP-SD method simultaneously. For an arbitrarily thick snow layer, thin slabs of a snow pack is analyzed a corresponding polarimetric N-port (representing different directions of scattering) S-matrix is generated. These S-matrices are cascaded using SSWaP-SD method to calculate the total forward and backward bistatic scattered fields in a fully coherent way. The simulation results of the backscattering from an arbitrary thick snow layer are presented.
机译:考虑了来自任意厚度的3D积雪的基于物理的全相干电磁(EM)散射模型。使用Lineal-Path函数与3D空间指数相关函数的结合来重构计算机生成的雪介质,以确保雪粒子的宏观连通性。使用统计S矩阵波在频谱域中传播(SSWaP-SD)以及基于离散偶极近似(DDA)的矩量法(MoM)代码,可以执行全相干EM计算。选择该方法是为了同时利用DDA的省时计算和SSWaP-SD方法的全相干性。对于任意厚的积雪层,分析了积雪的薄板,会生成相应的极化N端口(代表不同的散射方向)S矩阵。使用SSWaP-SD方法将这些S矩阵级联,以完全相干的方式计算总的前向和后向双静态散射场。给出了任意厚​​雪层向后散射的模拟结果。

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