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Polarimetric passive microwave remote sensing of wind vectors with foam-covered rough ocean surfaces

机译:具有泡沫覆盖的粗糙海洋表面的风向的极化被动微波遥感

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In this paper, polarimetric microwave emissions from wind-generated foam-covered ocean surfaces are investigated. The foam is treated as densely packed air bubbles coated with thin seawater coating. The absorption, scattering and extinction coefficients are calculated by Monte Carlo simulations of solutions of Maxwell equations of a collection of coated particles. The effects of boundary roughness of ocean surface are included by using the second-order small perturbation method (SPM) describing the reflection coefficients between foam and ocean. An empirical wavenumber spectrum is used to represent the small-scale wind-generated sea surfaces. The iterative method is employed to solve dense media radiative transfer (DMRT) equations, and is applied to calculate results of all four Stokes parameters of rough ocean surfaces. The theoretical results of four Stokes brightness temperatures with typical parameters of foam in passive remote sensing at 10.8 GHz, 19 GHz and 36.5 GHz are illustrated. The azimuth variations of polarimetric brightness temperature are calculated. Emission with various wind speed and foam layer thickness is studied. The results are also compared with those based on Quasi-Crystalline Approximation (QCA).
机译:在本文中,研究了由风力泡沫覆盖的海洋表面发出的极化微波辐射。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。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。该迭代方法用于求解致密介质辐射传递(DMRT)方程,并用于计算粗糙海洋表面的所有四个斯托克斯参数的结果。给出了在无源遥感中分别在10.8 GHz,19 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)的结果进行比较。

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