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首页> 外文期刊>Physics and chemistry of the earth >Upscaling discrete internal observations for obtaining catchment-averaged TOPMODEL parameters in a small Mediterranean mountain basin
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Upscaling discrete internal observations for obtaining catchment-averaged TOPMODEL parameters in a small Mediterranean mountain basin

机译:扩大离散内部观测值,以获取地中海小山区流域平均TOPMODEL参数

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Discrete observations on recession flows, local depth to the water table and the extent of saturated areas were used in the Vallcebre small research basin for obtaining the distribution functions of the TOPMODEL catchment parameters that drive the behaviour of the saturated store. Using this parameter information within GLUE framework, the robustness of discharge simulations was improved and the uncertainty of flow separation between two components was significantly reduced when compared with the results obtained with customary calibration with flow data at the outlet. Nevertheless, the analysis of the uncertainty in the determination of the local value of the topographic index at the piezometer location demonstrated that this may be a relevant limitation of the approach, particularly for high values of the topographic index, and a careful selection of the piezometer is recommended. The use of the extent of saturated areas provided the best and more representative results, although the simulated patterns of saturated areas did not match well the observed ones, because the role of local controls beyond the topographic index.
机译:在Vallcebre小型研究盆地中,对衰退流量,地下水位的局部深度和饱和区域的范围进行了离散观测,以获取驱动饱和存储行为的TOPMODEL集水参数的分布函数。与通过出口处的流量数据进行常规校准所获得的结果相比,在GLUE框架内使用此参数信息可以提高排放模拟的鲁棒性,并显着减少两个组件之间的流动分离的不确定性。尽管如此,对确定测压仪位置处的局部地形指数的不确定性的分析表明,这可能是该方法的一个局限性,特别是对于地形指数较高的情况,以及对测压仪的精心选择被推荐。尽管饱和区域的模拟模式与观察到的模式并不完全匹配,但使用饱和区域的范围提供了最佳且更具代表性的结果,因为局部控制的作用超出了地形指数。

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