首页> 外文会议>Geoscience and Remote Sensing Symposium, 1999. IGARSS '99 Proceedings. IEEE 1999 International >Polarimetric scattering coefficients of half-space heterogeneous medium
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Polarimetric scattering coefficients of half-space heterogeneous medium

机译:半空间非均质介质的极化散射系数

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Almost all natural media such as a rain, ice, fog, snow, clouds, leaves, forests, surface soil layer, agricultural plants, etc. can be considered as some kind of heterogeneous random medium embedded with nonspherical discrete particles. In this paper the polarimetric backscattering coefficients of half-space random medium are calculated for the purposes of the environmental remote sensing using polarimetric radars. The stochastic model of the half-space heterogeneous medium consists of a random current propagating in a hypothetical isotropic medium. The parameters of the model used in this paper are derived by the aid of strong permittivity fluctuation theory under a bilocal as well low-frequency approximations. The symmetry of scattering matrix F was proven in backscattering direction of measurement of scattered electromagnetic field in the atmosphere. It was shown that the polarimetric covariance matrix C consists of two polarimetric covariance matrices of unperturbed and random parts of scattered electromagnetic field. It was as well shown that in backscattering direction the scattering coefficients /spl sigma//sub hv/, /spl sigma//sub hhhv/, /spl sigma//sub hvvv/ are different from zero in general. The expressions of polarimetric backscattering scattering coefficients given in this paper are valid for arbitrary joint probability density function P(/spl theta/,/spl phi/) of scatterers spatial orientation. The obtained results can be used for the purposes of polarimetric remote sensing of heterogeneous natural media embedded with discrete scatterers having non spherical geometry.
机译:几乎所有自然介质,如雨,冰,雾,雪,云,树叶,森林,表层土壤层,农业植物等,都可以被视为嵌入了非球形离散颗粒的某种非均质随机介质。本文针对极化雷达进行环境遥感的目的,计算了半空间随机介质的极化反向散射系数。半空间异质介质的随机模型由在假设各向同性介质中传播的随机电流组成。本文所用模型的参数是在双局部以及低频近似下借助强介电常数波动理论导出的。在大气中散射电磁场的测量的反向散射方向上证明了散射矩阵F的对称性。结果表明,极化协方差矩阵C由散射电磁场的无扰动和随机部分的两个极化协方差矩阵组成。还表明,在反向散射方向上,散射系数/ spl sigma // sub hvv /,/ spl sigma // sub hhhv /,/ spl sigma // sub hvvv /通常不同于零。本文给出的偏振反向散射散射系数的表达式对于散射体空间取向的任意联合概率密度函数P(/ spl theta /,/ spl phi /)是有效的。所获得的结果可用于极化遥测异质自然介质的目的,该介质嵌入了具有非球形几何形状的离散散射体。

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