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Parameter uncertainty analysis for an operational hydrological model using residual-based and limits of acceptability approaches

机译:基于残差和可接受性极限的运行水文模型参数不确定性分析

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Parameter uncertainty estimation is one of the major challenges in hydrological modeling. Here we present parameter uncertainty analysis of a recently released distributed conceptual hydrological model applied in the Nea catchment, Norway. Two variants of the generalized likelihood uncertainty estimation (GLUE) methodologies, one based on the residuals and the other on the limits of acceptability, were employed. Streamflow and remote sensing snow cover data were used in conditioning model parameters and in model validation. When using the GLUE limit of acceptability (GLUE LOA) approach, a streamflow observation error of 25?% was assumed. Neither the original limits nor relaxing the limits up to a physically meaningful value yielded a behavioral model capable of predicting streamflow within the limits in 100?% of the observations. As an alternative to relaxing the limits, the requirement for the percentage of model predictions falling within the original limits was relaxed. An empirical approach was introduced to define the degree of relaxation. The result shows that snow- and water-balance-related parameters induce relatively higher streamflow uncertainty than catchment response parameters. Comparable results were obtained from behavioral models selected using the two GLUE methodologies.
机译:参数不确定性估计是水文建模的主要挑战之一。在这里,我们介绍了在挪威Nea流域应用的最新发布的分布式概念水文模型的参数不确定性分析。使用了广义似然不确定性估计(GLUE)方法的两种变体,一种基于残差,另一种基于可接受性极限。流量和遥感积雪数据用于条件模型参数和模型验证。当使用GLUE可接受极限(GLUE LOA)方法时,假定流量观测误差为25%。最初的限制或将限制放宽到物理上有意义的值都不能产生能够在观察值的100%以内的范围内预测流量的行为模型。作为放宽限制的替代方法,放宽了对模型预测百分比在原始限制内的要求。引入了经验方法来定义松弛程度。结果表明,与积雪和水平衡相关的参数比集水区响应参数引起的相对较高的流量不确定性。从使用两种GLUE方法选择的行为模型获得了可比的结果。

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