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Assimilation of remote sensing observations into a continuous distributed hydrological model: Impacts on the hydrologic cycle

机译:遥感观测分化成为连续分布水文模型的影响:对水文循环的影响

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摘要

A reliable estimation of soil moisture conditions is fundamental for discharges prediction and, consequently, for flood risk mitigation. Microwave remote sensing can be exploited to estimate soil moisture at large scale. These estimates can be used to enhance the predictions of hydrological models using Data Assimilation techniques and to reduce model uncertainties. This research tested the effects of the assimilation of three different satellite-derived soil moisture products (obtained from ASCAT acquisitions) in a distributed, physically based, hydrological model applied to three small Italian catchments. The products were firstly preprocessed, in order to be to be comparable with the state variables of the model. Subsequently they were assimilated by using different techniques: a simple Nudging applied at both model and satellite scale and the Ensemble Kalman Filter. Finally, observed discharges were compared with the modelled ones. The reanalysis was executed for a multi-year period ranging from July 2012 to June 2014.
机译:可靠估计土壤湿度条件是放电预测的基础,因此用于洪水风险减缓。微波遥感可以利用大规模估算土壤水分。这些估计可用于增强使用数据同化技术的水文模型的预测,并降低模型不确定性。该研究检测了在应用于三个小意大利集水区的分布式,物理基础的水文模型中的三种不同卫星衍生土壤水分产品(从ASCAT采集获得)的影响。首先预处理产品,以便与模型的状态变量相媲美。随后通过使用不同的技术同化它们:在模型和卫星秤上应用了一个简单的亮度,并施用了集合卡尔曼滤波器。最后,将观察到的放电与建模的放电进行比较。重新分析是在2012年7月至2014年6月到2014年7月的一个多年期间。

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