On the uncertainty of long-period return values of extreme daily precipitation

IF 3.3 Q2 ENVIRONMENTAL SCIENCES Frontiers in Climate Pub Date : 2024-03-15 DOI:10.3389/fclim.2024.1343072
Michael F. Wehner, Margaret L. Duffy, M. Risser, C. J. Paciorek, Dáithí A. Stone, P. Pall
{"title":"On the uncertainty of long-period return values of extreme daily precipitation","authors":"Michael F. Wehner, Margaret L. Duffy, M. Risser, C. J. Paciorek, Dáithí A. Stone, P. Pall","doi":"10.3389/fclim.2024.1343072","DOIUrl":null,"url":null,"abstract":"Methods for calculating return values of extreme precipitation and their uncertainty are compared using daily precipitation rates over the Western U.S. and Southwestern Canada from a large ensemble of climate model simulations. The roles of return-value estimation procedures and sample size in uncertainty are evaluated for various return periods. We compare two different generalized extreme value (GEV) parameter estimation techniques, namely L-moments and maximum likelihood (MLE), as well as empirical techniques. Even for very large datasets, confidence intervals calculated using GEV techniques are narrower than those calculated using empirical methods. Furthermore, the more efficient L-moments parameter estimation techniques result in narrower confidence intervals than MLE parameter estimation techniques at small sample sizes, but similar best estimates. It should be noted that we do not claim that either parameter fitting technique is better calibrated than the other to estimate long period return values. While a non-stationary MLE methodology is readily available to estimate GEV parameters, it is not for the L-moments method. Comparison of uncertainty quantification methods are found to yield significantly different estimates for small sample sizes but converge to similar results as sample size increases. Finally, practical recommendations about the length and size of climate model ensemble simulations and the choice of statistical methods to robustly estimate long period return values of extreme daily precipitation statistics and quantify their uncertainty.","PeriodicalId":33632,"journal":{"name":"Frontiers in Climate","volume":null,"pages":null},"PeriodicalIF":3.3000,"publicationDate":"2024-03-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Frontiers in Climate","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3389/fclim.2024.1343072","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0

Abstract

Methods for calculating return values of extreme precipitation and their uncertainty are compared using daily precipitation rates over the Western U.S. and Southwestern Canada from a large ensemble of climate model simulations. The roles of return-value estimation procedures and sample size in uncertainty are evaluated for various return periods. We compare two different generalized extreme value (GEV) parameter estimation techniques, namely L-moments and maximum likelihood (MLE), as well as empirical techniques. Even for very large datasets, confidence intervals calculated using GEV techniques are narrower than those calculated using empirical methods. Furthermore, the more efficient L-moments parameter estimation techniques result in narrower confidence intervals than MLE parameter estimation techniques at small sample sizes, but similar best estimates. It should be noted that we do not claim that either parameter fitting technique is better calibrated than the other to estimate long period return values. While a non-stationary MLE methodology is readily available to estimate GEV parameters, it is not for the L-moments method. Comparison of uncertainty quantification methods are found to yield significantly different estimates for small sample sizes but converge to similar results as sample size increases. Finally, practical recommendations about the length and size of climate model ensemble simulations and the choice of statistical methods to robustly estimate long period return values of extreme daily precipitation statistics and quantify their uncertainty.
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
关于极端日降水量长周期回归值的不确定性
利用大型气候模式模拟集合中美国西部和加拿大西南部的日降水率,比较了计算极端降水回归值及其不确定性的方法。针对不同的回归期,对回归值估算程序和样本大小在不确定性中的作用进行了评估。我们比较了两种不同的广义极值(GEV)参数估计技术,即 L-moments 和最大似然法(MLE),以及经验技术。即使对于非常大的数据集,使用 GEV 技术计算出的置信区间也比使用经验方法计算出的置信区间要窄。此外,更有效的 L-moments 参数估计技术在小样本量时的置信区间也比 MLE 参数估计技术窄,但最佳估计值却相似。需要注意的是,我们并没有说任何一种参数拟合技术都比另一种技术更适合估计长期回报值。虽然非稳态 MLE 方法可用于估算 GEV 参数,但 L-moments 方法却不适用。对不确定性量化方法进行比较后发现,在样本量较小的情况下,估算结果会有显著差异,但随着样本量的增加,结果会趋于相似。最后,就气候模式集合模拟的长度和规模以及统计方法的选择提出了实用建议,以稳健地估算极端日降水量统计的长期回归值并量化其不确定性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Frontiers in Climate
Frontiers in Climate Environmental Science-Environmental Science (miscellaneous)
CiteScore
4.50
自引率
0.00%
发文量
233
审稿时长
15 weeks
期刊最新文献
Gender vulnerability assessment to inform gender-sensitive adaptation action: a case study in semi-arid areas of Mali Climatology, trends, and future projections of aerosol optical depth over the Middle East and North Africa region in CMIP6 models Projections of the Adriatic wave conditions under climate changes Microbe-mineral interactions within kimberlitic fine residue deposits: impacts on mineral carbonation Socio-economic implications of forest-based biofuels for marine transportation in the Arctic: Sweden as a case study
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1