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首页> 外文期刊>Journal of hydrologic engineering >Bivariate Frequency Analysis of Hydrological Drought Using a Nonstationary Standardized Streamflow Index in the Yangtze River
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Bivariate Frequency Analysis of Hydrological Drought Using a Nonstationary Standardized Streamflow Index in the Yangtze River

机译:基于非平稳标准化流量指数的长江水文干旱双变量频率分析

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In order to reassess the hydrological drought in the Yangtze River under changing environment, a nonstationary standardized streamflow index was proposed in this study to fit the streamflow series at Yichang station; time and a modified reservoir index were introduced as covariates to assess the effect of reservoir regulation. The copula method was applied for bivariate modeling of drought duration and severity, in which joint and conditional return periods were considered for drought risk assessment. The results indicated that the monthly streamflow series at Yichang station have undergone great changes and the stationary assumption is no longer valid. The drought severity was more severe with its marginal distribution changed from the generalized extreme value to gamma when considering nonstationary properties. The Joe copula was selected for bivariate frequency analysis, and the correlation coefficient between drought characteristics increased in nonstationary models. Using the conditional return period, the model with reservoir index as covariate reported a worse drought condition compared with the stationary model, implying that the reservoirs may deteriorate the downstream hydrological drought at the Yichang station. By contrast, the time covariate may underestimate the drought risk. The nonstationary index is capable for drought modeling in the Yangtze River, and can be a useful tool in further research.
机译:为了重新评估变化环境下的长江水文干旱,本研究提出了一种非平稳标准化流量指数,以适应宜昌站的流量序列。引入时间和修改后的储层指数作为协变量,以评估储层调节的效果。 copula方法用于干旱持续时间和严重程度的双变量建模,其中考虑联合和有条件的恢复期进行干旱风险评估。结果表明,宜昌站的月流量序列发生了很大的变化,固定假设不再有效。考虑到非平稳性时,干旱严重程度更为严重,其边际分布从广义极值变为γ。选择Joe copula进行双变量频率分析,在非平稳模型中干旱特征之间的相关系数增加。使用条件回归期,以水库指数为协变量的模型与稳定模型相比,报告的干旱条件更差,这意味着水库可能使宜昌站的下游水文干旱恶化。相反,时间协变量可能低估了干旱风险。非平稳指数可以用于长江中下游地区的干旱建模,并且可以作为进一步研究的有用工具。

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