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首页> 外文期刊>Journal of hydrometeorology >Regional parameter estimation of the VIC land surface model: methodology and application to river basins in China
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Regional parameter estimation of the VIC land surface model: methodology and application to river basins in China

机译:VIC地表模型的区域参数估计:方法及在中国流域的应用

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This paper presents a methodology for regional parameter estimation of the three-layer Variable Infiltration Capacity (VIC-3L) land surface model with the goal of improving the streamflow simulation for river basins in China. This methodology is designed to obtain model parameter estimates from a limited number of calibrated basins and then regionalize them to uncalibrated basins based on climate characteristics and large river basin domains, and ultimately to continental China. Fourteen basins from different climatic zones and large river basins were chosen for model calibration. For each of these basins, seven runoff-related model parameters were calibrated using a systematic manual calibration approach. These calibrated parameters were then transferred within the climate and large river basin zones or climatic zones to the uncalibrated basins. To test the efficiency of the parameter regionalization method, a verification study was conducted on 19 independent river basins in China. Overall, the regionalized parameters, when evaluated against the a priori parameter estimates, were able to reduce the model bias by 0.4%-249.8% and relative root-mean-squared error by 0.2%-119.1% and increase the Nash-Sutcliffe efficiency of the streamflow simulation by 1.9%-31.7% for most of the tested basins. The transferred parameters were then used to perform a hydrological simulation over all of China so as to test the applicability of the regionalized parameters on a continental scale. The continental simulation results agree well with the observations at regional scales, indicating that the tested regionalization method is a promising scheme for parameter estimation for ungauged basins in China.
机译:本文提出了一种三层可变入渗能力(VIC-3L)地表模型区域参数估计的方法,目的是改善中国流域的水流模拟。此方法旨在从有限数量的已校准盆地中获取模型参数估计值,然后根据气候特征和大河流域域将其区域化为未校准盆地,并最终分布到中国大陆。选择了来自不同气候区的十四个盆地和大型流域进行模型校准。对于这些流域中的每个流域,使用系统的手动校准方法对七个与径流有关的模型参数进行了校准。然后,将这些校准后的参数在气候区和大河流域或气候区中传输到未校准的流域。为了验证参数分区方法的有效性,对中国19个独立流域进行了验证研究。总体而言,与先验参数估计值相比,区域化参数能够将模型偏差降低0.4%-249.8%,相对均方根误差降低0.2%-119.1%,并提高Nash-Sutcliffe效率大多数测试盆地的流量模拟为1.9%-31.7%。然后,将转移的参数用于在整个中国进行水文模拟,以测试区域参数在大陆范围内的适用性。大陆模拟结果与区域尺度的观测结果吻合得很好,这表明,经过测试的区域化方法是对中国未充填盆地进行参数估算的有前途的方案。

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