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Separately accounting for uncertainties in rainfall and runoff: Calibration of event-based conceptual hydrological models in small urban catchments using Bayesian method

机译:分别考虑降雨和径流的不确定性:使用贝叶斯方法对小城市集水区基于事件的概念水文模型进行校准

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摘要

Uncertainty analysis of hydrological models is usually based on model calibration, and the Bayesian method is a popular way to evaluate the uncertainty. The traditional Bayesian method usually uses lumped model residuals to form the likelihood function, where uncertainty in inputs (rainfall) is not explicitly addressed. This paper compares three approaches based on Bayesian inferences, considering rainfall uncertainty either implicitly or explicitly in calibration. Consistent parameter estimation and reliable quantification of predictive uncertainty are mainly examined. When rainfall uncertainty is explicitly treated in calibration, several rainfall observations at one-minute time steps are grouped to share one multiplier to consider the possible observation errors. The appropriate grouping strategy that balances the representativeness and the complexity of the problem is suggested. The application of the methods considered in this study focuses on small urban catchments (<200 ha) with a small temporal scale (min time step), in contrast to most literature studies dealing with larger catchments monitored at larger time steps. It is found that uncertainty in rainfall has a minor contribution to the total uncertainty in runoff estimation, and this minor role can be explained by the low pass filter effect of the linear reservoir model. However, the approach explicitly accounting for input uncertainty results in more informed knowledge for uncertainties related with hydrological model calibrations, which can possibly provide an estimation of uncertainty attributed to rainfall records. It should be noted that rainfall error estimates can compensate model structural uncertainty that is not explicitly addressed in this study.
机译:水文模型的不确定性分析通常基于模型校准,贝叶斯方法是评估不确定性的常用方法。传统的贝叶斯方法通常使用集总模型残差来形成似然函数,其中未明确解决输入不确定性(降雨)。本文比较了基于贝叶斯推论的三种方法,并在校准中隐含或显式考虑了降雨不确定性。主要检查一致的参数估计和预测不确定性的可靠量化。如果在校准中明确处理了降雨不确定性,则将在一分钟时间步长上的几个降雨观测结果进行分组,以共享一个乘数,以考虑可能的观测误差。建议适当的分组策略来平衡问题的代表性和复杂性。与大多数文献研究以较大的时间步长监测较大的流域相比,本研究中所考虑的方法的应用侧重于具有较小的时间尺度(最小时间步长)的小型城市流域(<200公顷)。结果表明,降雨不确定性对径流估算总不确定性的影响很小,这可以用线性储层模型的低通滤波效应来解释。但是,显式考虑输入不确定性的方法会导致对与水文模型校准有关的不确定性有更多的了解,这可能会提供降雨记录带来的不确定性估计。应当指出,降雨误差估计可以补偿本研究中未明确解决的模型结构不确定性。

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  • 来源
    《Water resources research》 |2013年第9期|5381-5394|共14页
  • 作者单位

    LGCIE, INSA Lyon, University of Lyon, FR-69621 Villeurbanne CEDEX, France;

    LGCIE, INSA Lyon, University of Lyon, Villeurbanne, France;

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