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Discharge and water-depth estimates for ungauged rivers: Combining hydrologic, hydraulic, and inverse modeling with stage and water-area measurements from satellites

机译:未吞噬河流的流量和水深估算:将水文,水力和逆模型与卫星的阶段和水域测量相结合

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摘要

Anticipating future global freshwater scarcity and providing mitigation require timely knowledge of spatiotemporal dynamics of discharge for gauged and, more challengingly, ungauged rivers. This study describes a coupled hydrologic (SWAT) and hydraulic (XSECT) modeling approach set in a genetic algorithm framework for estimating discharge and water depth for ungauged rivers from space. The method was tested in the Red River of the North basin by comparing simulated discharges and depths from 2006 to 2010 to in situ observations from across the basin. Results showed that calibration using only remotely sensed data (i.e., water levels from ENVISAT altimetry and water extents from LANDSAT) along the main stem of the Red River yielded daily and monthly estimates of river discharge, which correlated to measured discharges at three gaging stations on the main stem with R-2 values averaging 0.822 and 0.924, respectively. The comparisons of modeled and measured discharges were also extended to smaller tributaries, yielding a mean R-2 of 0.809 over seven gaging stations. The modeling approach also provided estimates of water depth that correlated to observations at four stations with an average R-2 of 0.831. We conclude that the integrated modeling approach is able to estimate discharge and water depth from space for larger ungauged rivers. This study also implies that in situ discharge data may not be necessary for successful hydrologic model calibration.
机译:预测未来全球淡水短缺并提供缓解措施,需要及时了解经过测量的,以及更具挑战性的未加水河流的排放时空动态。这项研究描述了在遗传算法框架中设置的水文(SWAT)和水力(XSECT)耦合建模方法,用于估算空间中未引流河流的流量和水深。通过将2006年至2010年的模拟流量和深度与整个流域的现场观测值进行比较,在北流域的红河中对该方法进行了测试。结果表明,仅使用遥感数据(即,ENVISAT测高仪的水位和LANDSAT的水位)沿红河干流进行校准,就可以得出每日和每月的河流流量估算值,这与在三个测站上测得的流量有关主干的R-2值分别平均为0.822和0.924。模拟排放量和测量排放量的比较也扩展到较小的支流,七个测量站的平均R-2为0.809。该建模方法还提供了与四个站点的观测值相关的水深估计,平均R-2为0.831。我们得出的结论是,综合建模方法能够估算出较大的未引流河流的空间流量和水深。这项研究还暗示,对于成功的水文模型校准来说,原位流量数据可能不是必需的。

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  • 来源
    《Water resources research》 |2015年第8期|6017-6035|共19页
  • 作者单位

    Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA;

    Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA;

    Natl Cent Univ, Ctr Space & Remote Sensing Res, Taoyuan, Taiwan;

    Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA;

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