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首页> 外文期刊>Advances in Water Resources >Revisiting flood peak distributions: A pan-Canadian investigation
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Revisiting flood peak distributions: A pan-Canadian investigation

机译:重新审视洪峰分布:泛加拿大调查

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摘要

Safe and cost-effective design of infrastructures, such as dams, bridges, highways, often requires knowing the magnitude and frequency of peak floods. The Generalized Extreme Value distribution (G epsilon V) prevailed in flood frequency analysis along with distributions comprising location, scale, and shape parameters. Here we explore alternative models and propose power-type models, having one scale and two shape parameters. The Burr type III (BrIII) and XII (BrXII) distributions are compared against the G epsilon V in 1088 streamflow records of annual peaks across Canada. A generic L-moment algorithm is devised to fit the distributions, also applicable to distributions without analytical L-moment expressions. The analysis shows: (1) the models perform equally well when describing the observed annual peaks; (2) the right tail appears heavier in the BrIII and BrXII models leading to larger streamflow predictions when compared to those of G epsilon V; (3) the G epsilon V predicts upper streamflow limits in 39.1% of the records-these limits have realistic exceedance probabilities based on the other two models; (4) the tail heaviness estimation seems not robust in the G epsilon V case when compared to the BrIII and BrXII models and this could challenge G epsilon V's reliability in predicting streamflow at large return periods; and, (5) regional variation is observed in the behaviour of flood peaks across different climatic regions of Canada. The findings of this study reveal potential limitations in using the G epsilon V for flood frequency analysis and suggest the BrIII and BrXII as consistent alternatives worth exploring.
机译:安全性和经济高效的基础设施设计,如水坝,桥梁,高速公路,通常需要了解峰洪水的幅度和频率。广义极值分布(G epsilon V)在洪水频率分析中持续,以及包括位置,尺度和形状参数的分布。在这里,我们探索替代模型,并提出具有一个规模和两个形状参数的功率型模型。将毛刺III型(BRIII)和XII(BRXII)分布与加拿大跨越每年峰的1088年流出记录中的G epsilon v比较。通常设计了一种通用的L-MOWER算法以适应分布,也适用于没有分析L-MOWER表达的分布。分析显示:(1)在描述观察到的年峰时,模型同样表现出; (2)与G Epsilon V相比,BRIII和BRXII模型中的右尾部在BRIII和BRXII模型中出现较大,导致更大的流流预测; (3)G epsilon V预测39.1%的记录中的上流流限制 - 这些限制基于其他两个模型的实际超标概率; (4)与BRIII和BRXII模型相比,尾部沉重估计似乎在G epsilon V案例中似乎不稳定,这可能会挑战G epsilon V在大返回时期预测流流程时的可靠性;并且(5)在加拿大不同气候区域的洪水峰的行为中观察到区域变异。该研究的结果揭示了使用G ePSilon V用于洪水频率分析的潜在限制,并表明BRIII和BRXII作为值得探索的一致替代品。

著录项

  • 来源
    《Advances in Water Resources 》 |2020年第11期| 103720.1-103720.12| 共12页
  • 作者单位

    Univ Saskatchewan Dept Civil Geol & Environm Engn Saskatoon SK Canada|Global Inst Water Secur 101-121 Res Dr Saskatoon SK S7N 1K2 Canada|Natl Water Res Ctr Drainage Res Inst Shoubra El Kheima Egypt;

    Univ Saskatchewan Dept Civil Geol & Environm Engn Saskatoon SK Canada|Global Inst Water Secur 101-121 Res Dr Saskatoon SK S7N 1K2 Canada|Czech Univ Life Sci Prague Fac Environm Sci Prague Czech Republic;

    Univ Saskatchewan Dept Civil Geol & Environm Engn Saskatoon SK Canada|Global Inst Water Secur 101-121 Res Dr Saskatoon SK S7N 1K2 Canada;

    McMaster Univ Sch Geog & Earth Sci Hamilton ON Canada|McMaster Univ Dept Civil Engn Hamilton ON Canada;

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

    Flood peaks; Extreme value theory; GEV distribution; Burr type III distribution;

    机译:洪水峰;极值理论;GEV分布;毛刺III型分布;

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