Global Applicability of the Kappa Distribution for Rainfall Frequency Analysis

IF 4.6 1区 地球科学 Q2 ENVIRONMENTAL SCIENCES
Robert Strong, Olivia Borgstroem, Rory Nathan, Conrad Wasko, Declan O’Shea
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Quality checks and thresholds were used to remove erroneous and poor-quality data, retaining 20,500 stations with 50 or more years of data. 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Consistent with theoretical expectations, <span data-altimg=\"/cms/asset/1a96b52e-6d43-4f73-899d-be3c670df5d3/wrcr27658-math-0002.png\"></span><mjx-container ctxtmenu_counter=\"108\" ctxtmenu_oldtabindex=\"1\" jax=\"CHTML\" role=\"application\" sre-explorer- style=\"font-size: 103%; position: relative;\" tabindex=\"0\"><mjx-math aria-hidden=\"true\" location=\"graphic/wrcr27658-math-0002.png\"><mjx-semantics><mjx-mrow><mjx-mi data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic- data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\"><mjx-c></mjx-c></mjx-mi></mjx-mrow></mjx-semantics></mjx-math><mjx-assistive-mml display=\"inline\" unselectable=\"on\"><math altimg=\"urn:x-wiley:00431397:media:wrcr27658:wrcr27658-math-0002\" display=\"inline\" location=\"graphic/wrcr27658-math-0002.png\" xmlns=\"http://www.w3.org/1998/Math/MathML\"><semantics><mrow><mi data-semantic-=\"\" data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\">h</mi></mrow>$h$</annotation></semantics></math></mjx-assistive-mml></mjx-container> converges toward zero (i.e., toward the limiting GEV distribution) as the average number of rainfall events per year increases (here approximated by rain days). However, in arid regions with a limited number of annual storm events, we observe average values of <span data-altimg=\"/cms/asset/57f11d0d-1cc0-4f26-b5c8-494a53ff54dd/wrcr27658-math-0003.png\"></span><mjx-container ctxtmenu_counter=\"109\" ctxtmenu_oldtabindex=\"1\" jax=\"CHTML\" role=\"application\" sre-explorer- style=\"font-size: 103%; position: relative;\" tabindex=\"0\"><mjx-math aria-hidden=\"true\" location=\"graphic/wrcr27658-math-0003.png\"><mjx-semantics><mjx-mrow><mjx-mi data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic- data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\"><mjx-c></mjx-c></mjx-mi></mjx-mrow></mjx-semantics></mjx-math><mjx-assistive-mml display=\"inline\" unselectable=\"on\"><math altimg=\"urn:x-wiley:00431397:media:wrcr27658:wrcr27658-math-0003\" display=\"inline\" location=\"graphic/wrcr27658-math-0003.png\" xmlns=\"http://www.w3.org/1998/Math/MathML\"><semantics><mrow><mi data-semantic-=\"\" data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\">h</mi></mrow>$h$</annotation></semantics></math></mjx-assistive-mml></mjx-container> greater than zero, with a strong regional and climatic coherence in <span data-altimg=\"/cms/asset/f8ccd802-db91-4364-8148-8b9bad41dcde/wrcr27658-math-0004.png\"></span><mjx-container ctxtmenu_counter=\"110\" ctxtmenu_oldtabindex=\"1\" jax=\"CHTML\" role=\"application\" sre-explorer- style=\"font-size: 103%; position: relative;\" tabindex=\"0\"><mjx-math aria-hidden=\"true\" location=\"graphic/wrcr27658-math-0004.png\"><mjx-semantics><mjx-mrow><mjx-mi data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic- data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\"><mjx-c></mjx-c></mjx-mi></mjx-mrow></mjx-semantics></mjx-math><mjx-assistive-mml display=\"inline\" unselectable=\"on\"><math altimg=\"urn:x-wiley:00431397:media:wrcr27658:wrcr27658-math-0004\" display=\"inline\" location=\"graphic/wrcr27658-math-0004.png\" xmlns=\"http://www.w3.org/1998/Math/MathML\"><semantics><mrow><mi data-semantic-=\"\" data-semantic-annotation=\"clearspeak:simple\" data-semantic-font=\"italic\" data-semantic-role=\"latinletter\" data-semantic-speech=\"h\" data-semantic-type=\"identifier\">h</mi></mrow>$h$</annotation></semantics></math></mjx-assistive-mml></mjx-container>. Our results suggest that there is merit in using the K4D for modeling heavy tail behavior, particularly in regions with a small number of events per year. These findings will contribute to advancing statistical modeling techniques for extreme rainfall, benefiting hydrological modeling and risk assessments.","PeriodicalId":23799,"journal":{"name":"Water Resources Research","volume":"28 1","pages":""},"PeriodicalIF":4.6000,"publicationDate":"2025-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Water Resources Research","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1029/2024wr039035","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0

Abstract

Extreme rainfall events have profound implications across various sectors, necessitating accurate modeling to assess risks and devise effective adaptation strategies. The common practice of employing three-parameter probability distributions, such as the Generalized Extreme Value (GEV) and Pearson Type III distributions, in rainfall frequency analysis often encounters limitations in capturing rare, heavy-tailed events with a lack of consensus as to which distribution is the most applicable. In this study, we explore the applicability of the four-parameter Kappa distribution (K4D) for modeling extreme daily rainfalls using annual maxima from the Global Historical Climatology Network-Daily database. Quality checks and thresholds were used to remove erroneous and poor-quality data, retaining 20,500 stations with 50 or more years of data. The variation in the second shape parameter (h$h$) was examined across regime characteristics, geospatial regions, and climate regional groupings to identify where the K4D is best able to model extreme rainfalls. Consistent with theoretical expectations, h$h$ converges toward zero (i.e., toward the limiting GEV distribution) as the average number of rainfall events per year increases (here approximated by rain days). However, in arid regions with a limited number of annual storm events, we observe average values of h$h$ greater than zero, with a strong regional and climatic coherence in h$h$. Our results suggest that there is merit in using the K4D for modeling heavy tail behavior, particularly in regions with a small number of events per year. These findings will contribute to advancing statistical modeling techniques for extreme rainfall, benefiting hydrological modeling and risk assessments.
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来源期刊
Water Resources Research
Water Resources Research 环境科学-湖沼学
CiteScore
8.80
自引率
13.00%
发文量
599
审稿时长
3.5 months
期刊介绍: Water Resources Research (WRR) is an interdisciplinary journal that focuses on hydrology and water resources. It publishes original research in the natural and social sciences of water. It emphasizes the role of water in the Earth system, including physical, chemical, biological, and ecological processes in water resources research and management, including social, policy, and public health implications. It encompasses observational, experimental, theoretical, analytical, numerical, and data-driven approaches that advance the science of water and its management. Submissions are evaluated for their novelty, accuracy, significance, and broader implications of the findings.
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