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Polarization Orientation Angle and Scattering Characteristics of Steep Terrain

机译:陡峭地形的偏振取向角与散射特性

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In this paper, we address polarimetric radar scattering from steep terrain and its relation to polarization orientation angle (POA) by adopting a tilted surface model based on Bragg scattering. We found that, as the azimuthal slope increases, |VV| decreases at a faster rate than |HH|, they become equal, when POA is ±45°, and |HH|>|VV| afterwards. Contrasting to the general perception, the cross-pol |HV| does not always increase with azimuth slope, but reaches a maximum then decreases to zero. In addition, we investigate the effect of soil moisture on PolSAR scattering characteristics of steep terrain and the effect of vegetation over surface on POA estimation. The latter is demonstrated with NASA/JPL TOPSAR L-band PolSAR data and C-band InSAR data.
机译:在本文中,我们通过采用基于布拉格散射的倾斜表面模型来解决来自陡峭地形的极化雷达散射及其与极化取向角(POA)的关系。我们发现,随着方位角斜率的增加,| VV |当POA为±45°时,| HH |> | VV |下降的速率比| HH |快,它们变得相等。然后。与一般的认识相反,交叉极化| HV |并不总是随着方位角的倾斜而增加,而是达到最大值然后减小到零。另外,我们研究了土壤水分对陡峭地形的PolSAR散射特征的影响以及植被对POA估计的影响。后者通过NASA / JPL TOPSAR L波段PolSAR数据和C波段InSAR数据进行了演示。

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