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首页> 外文期刊>Hydrology research >Sensitivity analysis of Xinanjiang rainfall-runoff model parameters: a case study in Lianghui,Zhejiang province, China
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Sensitivity analysis of Xinanjiang rainfall-runoff model parameters: a case study in Lianghui,Zhejiang province, China

机译:新安江降雨径流模型参数敏感性分析-以浙江凉水为例

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摘要

The Xinanjiang rainfall-runoff model has been successfully applied in many humid and sub-humid areas in China since 1973. The wide application is due to the simple model structure, the clear physical meaning of the parameters and the well-defined model calibration procedure. However, due to a data scarcity problem and short runoff concentration time, its applications to small drainage basins are difficult. Therefore, we investigate the model application in Lianghui, a small drainage basin of Zhejiang province in China. By using generalized likelihood uncertainty estimation (GLUE) methodology, the sensitivity of parameters of Xinanjiang model was investigated. The data clearly showed that equif inality phenomenon was evident in both water balance parameter calibration and runoff routing parameter calibration procedures. The results showed that K (evapotranspiration conversion coefficient), C_s (recession constant in channel system) and S_m (areal free water storage capacity of surface soil) are the most sensitive parameters for the water balance parameter calibration while C_s, S_m and W_m (mean area tension water capacity) are the most sensitive parameters for runoff routing parameter calibration. The conclusion is favourable for understanding parameters of Xinanjiang model in order to provide valuable scientific information for simulating hydrological processes in small drainage basins.
机译:自1973年以来,新安江降雨径流模型已在中国许多湿润和半湿润地区成功应用。广泛的应用是由于模型结构简单,参数的物理含义清晰以及模型定义程序明确。但是,由于数据缺乏问题和径流集中时间短,将其应用于小型流域十分困难。因此,我们研究了该模型在中国浙江省小流域良汇的应用。利用广义似然不确定性估计(GLUE)方法,研究了新安江模型参数的敏感性。数据清楚地表明,在水平衡参数校准和径流径流参数校准程序中均存在明显的均等现象。结果表明,K(蒸发蒸腾转换系数),C_s(渠道系统的后退常数)和S_m(表层土壤的面积自由储水量)是水平衡参数校准最敏感的参数,而C_s,S_m和W_m(平均值)区域张力水容量)是径流路径参数校准最敏感的参数。该结论有利于了解新安江模型的参数,为模拟小流域水文过程提供有价值的科学信息。

著录项

  • 来源
    《Hydrology research》 |2012年第2期|p.123-134|共12页
  • 作者单位

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai university,Nanjing 210098,China,College of Hydrology and Water resources,Hohai university,Nanjing 210098,China;

    Nanjing Hydraulic Research institute,Nanjing 210029,China;

    College of Hydrology and Water resources,Hohai university,Nanjing 210098,China;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering,Hohai university,Nanjing 210098,China;

    College of Hydrology and Water resources,Hohai university,Nanjing 210098,China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    equifinality; lianghui basin; uncertainty; xinanjiang model;

    机译:EQ UI finality;两会把思念;uncertainty;新安江model;

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