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Orientation Angle Calibration for Bare Soil Moisture Estimation Using Fully Polarimetric SAR Data

机译:利用全极化SAR数据估算裸土水分的方向角标定

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This paper focuses on assessing the effectiveness of applying orientation angle calibration to polarimetric synthetic aperture radar (PolSAR) data for soil moisture estimation. We employ Cloude-decomposition-based method to estimate the orientation angle because it can relate a scatter-distributed pixel to its major component of an equivalent "pure target," use the Jet Propulsion Laboratory/Airborne Synthetic Aperture Radar L-band fully polarimetric data to validate the proposed method, and observe results in good agreement after orientation angle compensation is employed. Specifically, root mean square errors of measured radar backscattering coefficients σhh0 and σvv0 and copolarization ratio versus advanced integral equation model predictions are reduced significantly from 1.95, 1.33, and 2.03 dB to 1.30, 1.15, and 1.43 dB, respectively. The compensated copolarized backscattering coefficients are also used as inputs to a novel inversion model to estimate the dielectric factor Rhh and volumetric soil moisture mv. The results show that the estimation errors are reduced significantly from 0.075 to 0.054 and 0.056 to 0.041 for Rhh and mv, respectively. This paper demonstrates the advantage of orientation angle calibration as a preprocessing for estimating bare soil moisture, particularly in agricultural areas, and the preponderance of fully PolSAR data on soil moisture estimation over dual and single polarizations.
机译:本文着重评估将方位角校准应用于极化合成孔径雷达(PolSAR)数据进行土壤湿度估算的有效性。我们使用基于Cloude分解的方法来估计方向角,因为它可以将散布的像素与等效“纯目标”的主要成分相关联,使用喷气推进实验室/机载合成孔径雷达L波段全极化数据验证了该方法的有效性,并在采用定向角补偿后观察到了良好的一致性。具体来说,测得的雷达反向散射系数σhh0和σvv0的均方根误差以及共极化比与高级积分方程模型的预测分别从1.95、1.33和2.03 dB显着降低到1.30、1.15和1.43 dB。补偿后的共极化后向散射系数也用作新型反演模型的输入,以估算介电系数Rhh和土壤土壤水分mv。结果表明,Rhh和mv的估计误差分别从0.075降低到0.054和0.056降低到0.041。本文展示了定向角校准作为估算裸露土壤水分(尤其是在农业地区)的预处理的优势,以及充分的PolSAR数据在双极化和单极化条件下对土壤水分估算的优势。

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