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An inversion method based on multi-angular approaches for estimating bare soil surface parameters from RADARSAT-1

机译:基于多角度方法的反演方法从RADARSAT-1估算裸土表面参数

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摘要

The radar signal recorded by earth observation (EO) satellites is sensitive to soil moisture and surface roughness, which both influence the onset of runoff. This paper focuses on inversion of these parameters using a multi-angular approach based on RADARSAT-1 data with incidence angles of 35° and 47° (in mode S3 and S7). This inversion was performed with three backscatter models: Geometrical Optics Model (GOM), Oh Model (OM), and Modified Dubois Model (MDM), which were compared to obtain the best configuration. Mean absolute errors of 1.23, 1.12, and 2.08 cm for roughness expressed in rms height and for dielectric constant, mean absolute errors of 2.46 - equal to 3.88 (m~3m~(-3)) in volumetric soil moisture, - 4.95 - equal to 8.72 (m~3m~(-3)) in volumetric soil moisture - and 3.31 - equal to 6.03 (m~3m~(-3)) in volumetric soil moisture - were obtained for the MDM, GOM, and OM simulation, respectively. These results indicate that the MDM provided the most accurate data with minimum errors. Therefore, the latter inversion algorithm was applied to images, and the final results are presented in two different maps showing pixel and homogeneous zones for surface roughness and soil moisture.
机译:地球观测(EO)卫星记录的雷达信号对土壤水分和表面粗糙度敏感,这两个因素都会影响径流的开始。本文着重研究基于RADARSAT-1数据,入射角为35°和47°(在S3和S7模式下)的多角度方法对这些参数的反演。使用三个反向散射模型进行了反演:几何光学模型(GOM),欧姆模型(OM)和修正的Dubois模型(MDM),将它们进行比较以获得最佳配置。以rms高度表示的粗糙度和介电常数的平均绝对误差为1.23、1.12和2.08 cm,平均土壤湿度的绝对绝对值为2.46-等于3.88(m〜3m〜(-3)),-4.95-等于在MDM,GOM和OM模拟中,获得了土壤水分的8.72(m〜3m〜(-3))至8.72(m〜3m〜(-3))和3.31-等于土壤水分的6.03(m〜3m〜(-3)),分别。这些结果表明,MDM提供了最准确的数据,并且错误最少。因此,将后一种反演算法应用于图像,最终结果显示在两个不同的地图中,分别显示了表面粗糙度和土壤湿度的像素区域和均质区域。

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