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A possibilistic approach to soil moisture retrieval from ERS synthetic aperture radar backscattering under soil roughness uncertainty

机译:在土壤粗糙度不确定性下从ERS合成孔径雷达反向散射获取土壤水分的可行方法

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摘要

Radar remote sensing of bare soil surfaces has been shown to be very useful for retrieving soil moisture. However, the error on the retrieved value depends on the accuracy of the roughness parameters (RMS height and correlation length). Several studies have demonstrated that these parameters show a high variability within a field, and therefore a lot of soil roughness profiles need to be measured to obtain accurate estimates. However, in an operational mode, soil roughness measurements are not available and therefore, for different types of tillage, roughness parameters are ill known. Possibility theory offers a way of handling this type of uncertainty, by modeling roughness parameters by means of possibility distributions. Inverting the integral equation model then leads to a possibility distribution for soil moisture. After transforming these possibilities into probabilities, mean soil moisture values and the uncertainty thereupon (given by the standard deviation) are obtained. It is found that the uncertainty depends on the wetness state of the soil. An application of our possibilistic retrieval algorithm to field observations at two sites in Belgium and one site in Italy resulted in accurate soil moisture observations (RMS error less than 6 vol %).
机译:裸露的土壤表面的雷达遥感已被证明对于获取土壤水分非常有用。但是,取回值的误差取决于粗糙度参数(RMS高度和相关长度)的准确性。多项研究表明,这些参数在田间显示出较高的可变性,因此,需要测量许多土壤粗糙度剖面以获得准确的估计值。但是,在操作模式下,无法进行土壤粗糙度测量,因此,对于不同类型的耕作,粗糙度参数是未知的。可能性理论通过利用可能性分布对粗糙度参数进行建模,提供了一种处理此类不确定性的方法。然后将积分方程模型反演,得出土壤水分的可能性分布。将这些可能性转换为概率后,即可获得平均土壤湿度值及其不确定性(由标准偏差得出)。发现不确定性取决于土壤的湿润状态。将我们的可能性检索算法应用于比利时的两个站点和意大利的一个站点的现场观测结果,可以得到准确的土壤湿度观测值(RMS误差小于6 vol%)。

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