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Simulations of emissivity in passive microwave remote sensing with three-dimensional numerical solutions of Maxwell equations and fast algorithm.

机译:利用麦克斯韦方程组的三维数值解法和快速算法模拟无源微波遥感中的发射率。

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摘要

In the first part of the work, we developed coding for large-scale computation to solve 3-dimensional microwave scattering problem. Maxwell integral equations are solved by using MoM with RWG basis functions in conjunction with fast computation algorithms. The cost-effective solutions of parallel and distributed simulation were implemented on a low cost PC cluster, which consists of 32 processors connected to a fast Ethernet switch. More than a million of surface current unknowns were solved at unprecedented speeds. Accurate simulations of emissivities and bistatic coefficients from ocean and soil were achieved. Exponential correlation function and ocean spectrum are implementd for generating soil and ocean surfaces. They have fine scale features with large rms slope. The results were justified by comparison with numerical results from original code, which is based on pulse basis function, and from analytic methods like SPM, and also with experiments. In the second part of the work, fully polarimetric microwave emissions from wind-generated foam-covered ocean surfaces were investigated. The foam is treated as densely packed air bubbles coated with thin seawater coating. The absorption, scattering and extinction coefficients were calculated by Monte Carlo simulations of solutionsof Maxwell equations of a collection of coated particles. The effects of boundary roughness of ocean surfaces were included by using the second-order small perturbation method (SPM) describing the reflection coefficients between foam and ocean. An empirical wave-number spectrum was used to represent the small-scale wind-generated sea surfaces. The theoretical results of four Stokes brightness temperatures with typical parameters of foam in passive remote sensing at 10.8 GHz, 19.0 GHz and 36.5 GHz were illustrated. The azimuth variations of polarimetric brightness temperature were calculated. Emission with various wind speed and foam layer thickness was studied. The results were also compared with those based on Quasi-Crystalline Approximation (QCA).
机译:在工作的第一部分中,我们开发了用于大规模计算的编码,以解决3维微波散射问题。通过使用具有RWG基函数的MoM结合快速计算算法来求解麦克斯韦积分方程。具有成本效益的并行和分布式仿真解决方案是在低成本PC群集上实现的,该群集由与快速以太网交换机相连的32个处理器组成。以前所未有的速度解决了超过一百万种表面电流未知数。精确模拟了海洋和土壤的发射率和双基地系数。实现了指数相关函数和海洋光谱以生成土壤和海洋表面。它们具有高均方根斜率的精细比例特性。通过与原始代码(基于脉冲基函数)的数值结果以及SPM等分析方法的数值结果进行比较,并与实验进行比较,证明了结果的合理性。在工作的第二部分中,研究了风力覆盖泡沫的海洋表面发出的全极化微波辐射。泡沫被视为密集的气泡,上面涂有薄薄的海水涂层。吸收,散射和消光系数是通过蒙特卡洛模拟方法计算的,该方法是对一系列包覆颗粒的麦克斯韦方程组的解进行求解。通过使用描述泡沫与海洋之间反射系数的二阶小扰动法(SPM),包括了海洋表面边界粗糙度的影响。用经验波数谱来表示小规模的风生海面。给出了在无源遥感中分别在10.8 GHz,19.0 GHz和36.5 GHz下使用泡沫的典型参数得出的四个斯托克斯亮度温度的理论结果。计算了偏振亮度温度的方位角变化。研究了不同风速和泡沫层厚度下的排放。还将结果与基于准晶体近似(QCA)的结果进行了比较。

著录项

  • 作者

    Zhou, Lin.;

  • 作者单位

    University of Washington.;

  • 授予单位 University of Washington.;
  • 学科 Engineering Electronics and Electrical.; Remote Sensing.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 118 p.
  • 总页数 118
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 无线电电子学、电信技术;遥感技术;
  • 关键词

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