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首页> 外文期刊>Journal of Hydrology >Extreme value analysis dilemma for climate change impact assessment on global flood and extreme precipitation
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Extreme value analysis dilemma for climate change impact assessment on global flood and extreme precipitation

机译:气候变化影响评估全球洪水和极端降水的极值分析

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摘要

A reliable estimation of hydrological extremes with potentially severe socio-economic impacts is of crucial importance for efficient planning and design of hydraulic structures. Extreme value theory provides a firm theoretical foundation for the statistical modelling of extreme hydrological events. The dilemma in the modelling is on whether to use block maxima (BM) or peak-over-threshold (POT) method, each with its own cons and pros. It remains unexplored to what extent future projected changes in extreme hydrological events are influenced by the method choice, especially when some simplifications are made to lessen the computational burden for largescale studies. This study addresses this research question by a comparative analysis between the BM and POT methods on future climate change impact on global flood and extreme precipitation. The extreme precipitation analysis is performed using 24 CMIP5 general circulation models (GCMs), while the flood analysis is based on a multi-model ensemble of 20 members including five global impact models forced by four CMIP5 GCMs. The results reveal that the BM and POT methods agree on the sign of changes in flood and extreme precipitation intensities, but disagree on the magnitude. The discrepancy between the BM and POT results increases with event extremity. The difference also varies with season, where the difference in the global land area with increasing signals peaks in winter at the rates of 11% for extreme precipitation and in summer at the rates of 3.5% for flood.
机译:对具有潜在严重社会经济影响的水文极端情况进行可靠估计,对于水工结构的有效规划和设计至关重要。极值理论为极端水文事件的统计建模提供了坚实的理论基础。建模中的难题在于是否使用块极大值(BM)或峰值超过阈值(POT)方法,每种方法都有各自的优缺点。极端水文事件的未来预测变化在多大程度上受方法选择的影响,尤其是在进行一些简化以减轻大规模研究的计算负担时,仍有待探索。本研究通过对比分析BM和POT方法对未来气候变化对全球洪水和极端降水的影响来解决这一研究问题。极端降水分析使用24个CMIP5大气环流模型(GCM)进行,而洪水分析基于20个成员的多模型集合,包括由四个CMIP5 GCM强制的五个全球影响模型。结果表明,BM和POT方法在洪水和极端降水强度变化的迹象上一致,但在量级上不一致。BM和POT结果之间的差异随着事件的极端而增加。这种差异也随季节而变化,全球陆地面积的差异在冬季达到峰值,极端降水率为11%,洪水率为3.5%。

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