Separating the attributions of anthropogenic activities and climate change to streamflow and multivariate dependence analysis

IF 2.3 4区 地球科学
Amir Askari, Hossein Fathian, Alireza Nikbakht-Shahbazi, Hoshang Hasonizade, Narges Zohrabi, Mohammad Shabani
{"title":"Separating the attributions of anthropogenic activities and climate change to streamflow and multivariate dependence analysis","authors":"Amir Askari,&nbsp;Hossein Fathian,&nbsp;Alireza Nikbakht-Shahbazi,&nbsp;Hoshang Hasonizade,&nbsp;Narges Zohrabi,&nbsp;Mohammad Shabani","doi":"10.1007/s11600-024-01479-0","DOIUrl":null,"url":null,"abstract":"<div><p>Streamflow changes in basins are influenced by two significant factors: anthropogenic activities and climate change (AACC). Separating the attribution of each factor is crucial for managing water resources and economic, political, and social activities. In this study, the Hydrologic Engineering Center’s Hydrologic Modeling System (HEC-HMS) model is used to separate annual AACC attributions to streamflow changes in Iran's Karkheh basin. The trend-free pre-whitening Mann–Kendall (TFPW-MK) test is used to determine trends in annual precipitation, streamflow, and air temperature. Multivariate dependence analysis is performed for precipitation and streamflow changes and attributions of AACC to streamflow changes using different copula functions. The point of change in the annual streamflow series, identified by the double cumulative curve (DCC) and Pettitt test, occurred in 1999. Compared to the pre-change period, the average annual streamflow decreased by 42.3%. The results of the hydrologic model simulation showed that climate change and anthropogenic activities contributed to streamflow reduction by 36.9% and 63.1%, respectively. The results showed that the attributions of AACC to streamflow each year could be obtained based on the dependence analysis between precipitation changes, streamflow changes, and the attributions of AACC to streamflow changes with copula functions. The results showed that for a joint probability of 0.5, the values of attributions of AACC to streamflow with the maximum joint density are equal to −42 and −36 mm, respectively.</p></div>","PeriodicalId":6988,"journal":{"name":"Acta Geophysica","volume":"73 2","pages":"1947 - 1963"},"PeriodicalIF":2.3000,"publicationDate":"2024-11-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geophysica","FirstCategoryId":"89","ListUrlMain":"https://link.springer.com/article/10.1007/s11600-024-01479-0","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Streamflow changes in basins are influenced by two significant factors: anthropogenic activities and climate change (AACC). Separating the attribution of each factor is crucial for managing water resources and economic, political, and social activities. In this study, the Hydrologic Engineering Center’s Hydrologic Modeling System (HEC-HMS) model is used to separate annual AACC attributions to streamflow changes in Iran's Karkheh basin. The trend-free pre-whitening Mann–Kendall (TFPW-MK) test is used to determine trends in annual precipitation, streamflow, and air temperature. Multivariate dependence analysis is performed for precipitation and streamflow changes and attributions of AACC to streamflow changes using different copula functions. The point of change in the annual streamflow series, identified by the double cumulative curve (DCC) and Pettitt test, occurred in 1999. Compared to the pre-change period, the average annual streamflow decreased by 42.3%. The results of the hydrologic model simulation showed that climate change and anthropogenic activities contributed to streamflow reduction by 36.9% and 63.1%, respectively. The results showed that the attributions of AACC to streamflow each year could be obtained based on the dependence analysis between precipitation changes, streamflow changes, and the attributions of AACC to streamflow changes with copula functions. The results showed that for a joint probability of 0.5, the values of attributions of AACC to streamflow with the maximum joint density are equal to −42 and −36 mm, respectively.

Abstract Image

求助全文
约1分钟内获得全文 求助全文
来源期刊
Acta Geophysica
Acta Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.80
自引率
13.00%
发文量
251
期刊介绍: Acta Geophysica is open to all kinds of manuscripts including research and review articles, short communications, comments to published papers, letters to the Editor as well as book reviews. Some of the issues are fully devoted to particular topics; we do encourage proposals for such topical issues. We accept submissions from scientists world-wide, offering high scientific and editorial standard and comprehensive treatment of the discussed topics.
×
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
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
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 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信