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Uncertainty analysis of water availability assessment through the Budyko framework

机译:通过Budyko框架进行水可用性评估的不确定性分析

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Parametric Budyko method has been widely used to assess water availability under changing environment. Its single parameter (w) controlling the shape of the Budyko curve, is of critical importance to water availability assessment (WAA). Here, the water availability is defined as the ratio of evapotranspiration to precipitation in the context of Budyko hypothesis. As an unobserved variable, w is generally estimated through incorporating the long-term water-balance model and Budyko hypothesis, i.e. estimating w as a function of precipitation, runoff, and potential evapotranspiration over a long-term time series of these variables. Inevitably, the estimated value of w is subject to uncertainty resulting from hydro-meteorological records with limited size. Further, this uncertainty affects WAA in context of Budyko hypothesis. The uncertainty and its propagation issue is often overlooked in past research. In this paper, we develop a bootstrap-based algorithm to reveal aforementioned uncertainty. Moreover, a partial derivative-based sensitivity analysis is performed for understanding the propagation of w uncertainty on WAA. Three catchments located in the Yellow River Basin, China, are used as case study sites. Results indicate that there exists remarkable uncertainty in parameter w, which varies with the data length. The impact of such uncertainty on WAA increases quickly under the humid condition, thereafter reaches a peak under the mild condition, and decreases slowly under the arid condition. The reason behind this phenomenon is the largest sensitivity of WAA to parameter w under the mild climate condition. Moreover, a general analytical expression for determining the critical value of climate condition which maximizes the impact of parameter w uncertainty on WAA is derived in this paper. Results of this study can enhance the reliability and robustness of Budyko-based models.
机译:参数Budyko方法已被广泛用于评估在不断变化的环境下的水可用性。它的单个参数(W)控制Budyko曲线形状,对水可用性评估(WAA)至关重要。在此,水可用性定义为Budyko假设的背景下的蒸馏与降水的比率。作为一种未观察的变量,通常通过包含长期水平模型和Budyko假设,即估计W作为降水,径流和这些变量的长期时间序列的函数的函数。不可避免地,W的估计值受到尺寸有限的水流记录产生的不确定性。此外,这种不确定性在Budyko假设的背景下影响了WAA。过去的研究往往忽视了不确定性及其传播问题。在本文中,我们开发了一种基于引导的算法,以揭示上述不确定性。此外,对基于局部衍生的敏感性分析进行了解理解W不确定性对WAA的传播。三个集水区位于中国黄河流域,被用作案例研究网站。结果表明参数W中存在显着的不确定性,其随数据长度而变化。这种不确定性对潮湿条件下这种不确定性的影响在潮湿条件下快速增加,此后在温和条件下达到峰值,并且在干旱条件下缓慢降低。这种现象背后的原因是在温和气候条件下对参数W的最大敏感性。此外,在本文中推导出最大化参数W不确定性的气候条件临界值的一般分析表达。该研究的结果可以提高基于Budyko的模型的可靠性和鲁棒性。

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