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Soil Moisture Retrieval Using Data Cube Representation of Radar Scattering

机译:基于雷达散射数据立方体表示的土壤水分反演

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A time-series algorithm is proposed to retrieve surface (from surface down to 1 m depth) soil moisture using the simulated radar data. The time-series approach uses co-polarized (VV and HH) backscattering coefficient (a0) values. Temporal averaging is applied to reduce the radar measurement noise. To the extent that the surface roughness does not change within the time-series window, the reduction of the noise enables the retrieval of the roughness. With the roughness estimate, subsequently soil moisture is retrieved. The proposed retrieval is performed using 'data cubes'. The data cubes relate soil moisture and a0, and are lookup tables with the dimensions of soil moisture, roughness, and vegetation water content (VWC). The cubes are generated by the first-order small perturbation model and the discrete scatterer model for the grass vegetation. A Monte-Carlo analysis demonstrates that the soil moisture may be retrieved within the error better than 0.06cm3/cm3 up to about 3kg/m2 VWC using six time-series records, although presently assuming that the radar model correctly describes the surface scattering processes.
机译:提出了一种时间序列算法,利用模拟雷达数据检索地表(从地表到1 m深度)的土壤水分。时间序列方法使用同极化(VV和HH)反向散射系数(a0)值。应用时间平均以减少雷达测量噪声。就表面粗糙度在时间序列窗口内不改变的程度而言,噪声的减少使得能够恢复粗糙度。通过粗糙度估计,随后可以获取土壤水分。建议的检索是使用“数据立方体”执行的。数据多维数据集与土壤湿度和a0相关,并且是具有土壤湿度,粗糙度和植被含水量(VWC)尺寸的查找表。多维数据集是由草植被的一阶小扰动模型和离散散射模型生成的。蒙特卡洛分析表明,使用六个时间序列记录,在大约3kg / m2 VWC的情况下,可以在优于0.06cm3 / cm3的误差范围内恢复土壤水分,尽管目前假设雷达模型正确描述了表面散射过程。

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