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Retrieval of Soil Moisture Profile by Combined C-band Scatterometer Data and a Surface Hydrological Model

机译:C波段散射仪数据及地表水文模型检索土壤湿度曲线

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The objective of this work is to develop a method to use radar scatterometer data and a hydrological model in order to retrieve soil behaviour at a level greater than C-band microwave penetration depth. For microwave measurements a C-band FM-CW scatterometer has been employed in two campaigns; the device is able to provide backscattering coefficients in the range of +10 dB and -40 dB for incidence angles between 10° and 60°. Subsequently, microwave scatterometer data have been analysed to estimate their sensitivity to the soil moisture patterns of topsoil comparing them with ground truth measurements. For the validation of these radar data, a coupled heat and moisture balance model has been run to predict the hydrological behaviour of the same topsoil starting from point ground truth measurements. In a second run, soil moisture values derived from scatterometer data should have been used for the initialisation of the model. First attempts have been carried out to propagate the surface physical parameters to unreachable soil layers, such as vertical soil moisture profiles [1].
机译:这项工作的目的是开发一种使用雷达散射仪数据和水文模型的方法,以便在大于C波段微波穿透深度的水平下检索土壤行为。对于微波测量,两次广告系列采用了C波段FM-CW散射仪;该装置能够在+10dB和-40dB的范围内提供反向散射系数,对于10°和60°之间的入射角。随后,已经分析了微波散射仪数据以估计其对TopSoil的土壤水分模式的敏感性,将它们与地面真理测量进行比较。为了验证这些雷达数据,已经运行了耦合的热量和水分平衡模型来预测从点地面真理测量开始的同一表土的水文行为。在第二次运行中,源自散射仪数据的土壤湿度值应该用于模型的初始化。首先尝试将表面物理参数传播到不可达的土层,例如垂直土壤水分型材[1]。

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