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Assimilation of remote sensing and hydrological data using adaptive filtering techniques for watershed modelling

机译:利用自适应滤波技术对流域建模进行遥感和水文数据同化

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摘要

The knowledge of hydrological variables (e. g. soil moisture, evapotranspiration) are of pronounced importance in various applications including flood control, agricultural production and effective water resources management. These applications require the accurate prediction of hydrological variables spatially and temporally in watershed/basin. Though hydrological models can simulate these variables at desired resolution (spatial and temporal), often they are validated against the variables, which are either sparse in resolution (e. g. soil moisture) or averaged over large regions (e. g. runoff). A combination of the distributed hydrological model (DHM) and remote sensing (RS) has the potential to improve resolution. Data assimilation schemes can optimally combine DHM and RS. Retrieval of hydrological variables (e. g. soil moisture) from remote sensing and assimilating it in hydrological model requires validation of algorithms using field studies. Here we present a review of methodologies developed to assimilate RS in DHM and demonstrate the application for soil moisture in a small experimental watershed in south India.
机译:在包括防洪,农业生产和有效水资源管理在内的各种应用中,水文变量(例如土壤湿度,蒸散量)的知识是非常重要的。这些应用要求在流域/盆地中在空间和时间上准确预测水文变量。尽管水文模型可以在所需的分辨率(空间和时间)上模拟这些变量,但是常常对变量进行验证,这些变量要么分辨率稀疏(例如土壤湿度),要么在较大区域平均(例如径流)。分布式水文模型(DHM)和遥感(RS)的组合具有提高分辨率的潜力。数据同化方案可以最佳地组合DHM和RS。从遥感中检索水文变量(例如土壤湿度)并将其同化到水文模型中,需要使用实地研究对算法进行验证。在这里,我们将介绍为吸收DHM中的RS而开发的方法学,并论证在印度南部一个小实验流域中土壤水分的应用。

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