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Estimation of parameters in a distributed precipitation-runoff model for Norway

机译:挪威分布式降雨-径流模型中参数的估计

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A distributed version of the HBV-model using 1 km(2) grid cells and daily time step was used to simulate runoff from the entire land surface of Norway for the period 1961-1990. The model was sensitive to changes in small scale properties of the land surface and the climatic input data, through explicit representation of differences between model elements, and by implicit consideration of sub-grid variations in moisture status. A geographically transferable set of model parameters was determined by a multi-criteria calibration strategy, which simultaneously minimised the residuals between model simulated and observed runoff from 141 Norwegian catchments located in areas with different runoff regimes and landscape characteristics. Model discretisation units with identical landscape classification were assigned similar parameter values. Model performance was evaluated by simulating discharge from 43 independent catchments. Finally, a river routing procedure using a kinematic wave approximation to open channel flow was introduced in the model, and discharges from three additional catchments were calculated and compared with observations. The model was used to produce a map of average annual runoff for Norway for the period 1961 1990. [References: 49]
机译:使用1 km(2)网格单元和每日时间步长的HBV模型的分布式版本用于模拟1961-1990年期间挪威整个陆地表面的径流。该模型通过显式表示模型元素之间的差异以及隐含考虑子网格中水分状况的变化,对土地表面和气候输入数据的小规模属性变化敏感。通过多准则校准策略确定了可在地理上转移的一组模型参数,该策略同时最小化了来自不同径流区域和景观特征区域的141个挪威流域的模拟径流和观测径流之间的残差。具有相同景观分类的模型离散化单元分配了相似的参数值。通过模拟43个独立流域的排放来评估模型性能。最后,在模型中引入了使用运动波近似法进行明渠水流的河道调度程序,并计算了另外三个集水区的流量并将其与观测值进行比较。该模型用于绘制1961 1990年期间挪威的年平均径流量图。[参考文献:49]

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