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Flood Wave Superposition Analysis Using Quantitative Matching Patterns of Peak Magnitude and Timing in Response to Climate Change

机译:洪波叠加分析使用峰值幅度和时序的定量匹配模式,以应对气候变化

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摘要

Flood wave superposition (FWS) of upstream and tributary rivers, as a typical compound hydrological event, may lead to considerable downstream flood hazards. In spite of this, the quantitative identification of FWS classification so far remains elusive. In this study, we quantitatively examined the typical matching patterns of FWS based on flood peak magnitude and timing between the upstream and tributary discharge, to evaluate the flood severity for both present-day conditions and future climate projections. The future FWS projection was realized using hydrological modeling coupled with multiple outputs of global climate models (GCMs) under the Representative Concentration Pathway (RCP) 2.6 and 8.5 emission scenarios. A triple point of discharge stations, including upstream, downstream and tributary stations, located at a river confluence of the Poyang Lake Basin, China, was selected as the study area. The results revealed that the frequency of perfect temporal matching (0-day time lag) of projected peaks between upstream and tributary floods increased from 61% in the reference period to 68% and 66% in the future under RCPs 2.6 and 8.5, respectively. Furthermore, both the future numbers and frequencies of the projected peaks between upstream and tributary floods with both perfect temporal and magnitude matching (the classification associated with the most damage in FWS) would substantially increase across all GCMs under RCPs 2.6 and 8.5. These findings indicate that future FWS is expected to experience increasing severity due to the changing climate under no matter RCP 2.6 or 8.5 emission scenarios. Overall, it is suggested that effective adaptation strategies be developed in order to stagger the timing of upstream and tributary floods in the future.
机译:上游和支流河流的洪波叠加(FWS)作为典型的复合水文事件,可能导致相当大的下游洪水危害。尽管如此,到目前为止,FWS分类的定量识别仍然是难以捉摸的。在这项研究中,我们根据上游和支流放电之间的洪水峰值和时序定量地检查了FWS的典型匹配模式,以评估当今条件和未来的气候预测的洪水严重程度。利用水文建模实现了未来的FWS投影,其在代表浓度途径(RCP)2.6和8.5发射方案下的全球气候模型(GCMS)的多个输出。选择了位于中国鄱阳湖盆地河流交汇处的上游,下游和支流站的三重排放站被选为研究区。结果表明,上游和支流洪水之间的预定峰值(0天时间滞后)的频率从参考时期的61%增加到& 68%和在RCPS 2.6和8.5下,将来的66%分别为66%。此外,既有完美的时间和幅度匹配的上游和支流泛洪叶之间的未来数量和频率都会与完美的时间和级别匹配(与FWS中最大部分损坏相关的分类)将在RCPS 2.6和8.5下的所有GCM上显着增加。这些调查结果表明,由于无论率为RCP 2.6或8.5发射方案,预计未来的FW可能会因不断变化的气候而越来越严重。总体而言,建议制定有效的适应策略,以便在未来的上游和支流洪水的时机交错。

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  • 来源
    《Water Resources Management》 |2021年第8期|2409-2432|共24页
  • 作者单位

    North China Elect Power Univ Sch Water Resources & Hydropower Engn Beijing 102206 Peoples R China;

    Wuhan Univ State Key Lab Water Resources & Hydropower Engn S Wuhan 430072 Peoples R China;

    Univ Oslo Dept Geosci POB 1047 N-0316 Oslo Blindern Norway;

    Wuhan Univ State Key Lab Water Resources & Hydropower Engn S Wuhan 430072 Peoples R China;

    North China Elect Power Univ Sch Water Resources & Hydropower Engn Beijing 102206 Peoples R China;

    North China Elect Power Univ Sch Water Resources & Hydropower Engn Beijing 102206 Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Climate change; Flood projection; Compound events; Hydrological modeling; GCMs;

    机译:气候变化;洪水投影;复合事件;水文建模;GCMS;

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