A polarimetric two-scale model for soil moisture retrieval

A. Iodice, A. Natale, D. Riccio
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引用次数: 3

Abstract

A polarimetric two-scale surface scattering model employed to retrieve the surface parameters of bare soils from polarimetric SAR data is proposed. The scattering surface is considered as composed of slightly rough randomly tilted facets, for which the Small Perturbation Method holds. The facet random tilt causes a random variation of the local incidence angle, and a random rotation of the local incidence plane around the line of sight, which in turn causes a random rotation of the facet scattering matrix. Unlike other similar already existing approaches, our method considers both these effects. The proposed scattering model is then used to retrieve bare soil moisture and (large-scale) roughness from the co-polarized and cross-polarized ratios. The performances of the resulting retrieval algorithm is finally assessed by comparing obtained results to “in situ” measurements. To this aim, data from Little Washita campaign available in literature is employed.
土壤水分反演的极化双尺度模型
提出了一种极化双尺度表面散射模型,用于从极化SAR数据中检索裸露土壤的表面参数。散射表面被认为是由稍微粗糙的随机倾斜面组成的,小摄动法适用于此。面随机倾斜引起局部入射角的随机变化,局部入射角平面围绕瞄准线的随机旋转,从而引起面散射矩阵的随机旋转。与其他类似的现有方法不同,我们的方法同时考虑了这两种影响。然后,利用所提出的散射模型从共极化和交叉极化比中检索裸地土壤湿度和(大尺度)粗糙度。最后通过将获得的结果与“原位”测量结果进行比较来评估所得到的检索算法的性能。为此,本文采用了文献中提供的Little Washita campaign数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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