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Estimation of Vegetation Parameters of Water Cloud Model for Global Soil Moisture Retrieval Using Time-Series L-Band Aquarius Observations

机译:利用时间序列L波段水瓶座观测值估算全球土壤水分反演的水云模型的植被参数

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Using Aquarius middle beam scatterometer observations, the vegetation parameters of the water cloud model at large scale are estimated and applied to global soil moisture retrieval. Vegetation backscattering is derived using two models: Oh model is used to describe the scattering from bare soil surface, while the water cloud model is implemented to account for the effect of vegetation canopy. The vegetation parameters are estimated by minimizing the deviations between the Aquarius scatterometer observations and backscatter coefficients simulated by the water cloud model. The RMSE is less than 2 dB for both copolarizations and correlation is strong ( CC>0.6) in most areas. The vegetation parameters were used to retrieve global soil moisture from Aquarius radar data. The comparisons with the Aquarius soil moisture product derived from the Aquarius radiometer observations show low ubRMSE ( 0.06cm3/cm3) and strong correlation ( CC>0.6) in most parts of the world. The impact of errors in input parameters of the water cloud model on the vegetation parameter estimation was assessed by using a Monte–Carlo simulation. The algorithm converges to the true values of the parameters when the input data is noise-free or only the radar measurement error is introduced. It was found that the errors in vegetation parameter are sensitive to the errors in input soil moisture. The errors in two vegetation parameters counteract each other to decrease the error of backscattering simulation. This study demonstrates that the water cloud model could be applied to global scatterometer observations to retrieve soil moisture if the vegetation parameters are appropriately set.
机译:利用水瓶座中波束散射仪的观测结果,可以大规模估算水云模型的植被参数,并将其应用于全球土壤水分的反演。植被反向散射的推导有两个模型:Oh模型用于描述裸露土壤表面的散射,而水云模型用于解释植被冠层的影响。通过最小化水瓶散射仪观测值与水云模型模拟的反向散射系数之间的偏差来估算植被参数。对于共极化,RMSE均小于2 dB,并且在大多数地区,相关性很强(CC> 0.6)。植被参数用于从水瓶座雷达数据中检索全球土壤湿度。与水瓶座辐射计观测到的水瓶座土壤水分产物的比较表明,在世界大多数地区,其ubRMSE低(0.06cm3 / cm3),并且相关性强(CC> 0.6)。通过使用蒙特卡洛模拟评估了水云模型输入参数中的误差对植被参数估计的影响。当输入数据无噪声或仅引入雷达测量误差时,该算法收敛到参数的真实值。发现植被参数误差对输入土壤水分的误差敏感。两个植被参数中的误差相互抵消,以减少反向散射模拟的误差。这项研究表明,如果适当设置植被参数,则可以将水云模型应用于全局散射仪观测以检索土壤水分。

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