Quantitative Assessment of Anthropogenic Activities on Precipitation–Flood Relations in the Middle-Lower Reaches of the Yangtze River Since the 21st Century

IF 2.9 3区 地球科学 Q1 Environmental Science Hydrological Processes Pub Date : 2024-12-25 DOI:10.1002/hyp.70035
Jiahao Xu, Zhiping Zhang, Junwei Chen, Zhongwei Shen, Xin Jia
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Abstract

Quantitatively distinguishing between climate change and anthropogenic activities is crucial for flood management in the middle-lower reaches of the Yangtze River (MLRYR). However, the quantitative contribution of climate change and anthropogenic activities to flood occurrences in the region over long time scales (spanning more than one climatic state) and across extensive spatial areas remains unclear. This study aims to address such issue by analysing runoff data from 12 hydrological stations in the MLRYR from 1961 to 2020. By combining the Peak Over Threshold (POT) method with the detection of flood event initiation and termination days, we analysed changes in mean annual flood duration days (MAFD) across two distinct periods: 1961–1987 (Phase I) and 2001–2020 (Phase II). Our results demonstrate a significant positive correlation between precipitation and flood in the MLRYR throughout the study period, though this correlation is weaker in Phase II compared to Phase I. By applying the double mass curve method, we quantified the contributions of climate change and anthropogenic activities to changes in MAFD in the MLRYR, comparing the period of rapid urbanisation since the 21st century to Phase I, when urbanisation was at its initial stage. The results indicate that anthropogenic activities have significantly suppressed average annual flood occurrences in Phase II, with contribution rates ranging from 118% to 199%. Conversely, changes in precipitation have positively influenced flood occurrences in Phase II, with contribution rates ranging from 18% to 99%. The extensive construction of hydraulic engineering has played a crucial role in regulating the runoff of the main and tributary rivers in the MLRYR, thereby weakening the precipitation–flood relations since the 21st century. This study suggests that the continued construction of hydraulic engineering in the MLRYR may remain a crucial measure for mitigating the increased flood risks associated with global warming and accelerated urbanisation in the future.

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21世纪以来长江中下游降水—洪水关系的人为活动定量评价
定量区分气候变化与人为活动对长江中下游洪水管理具有重要意义。然而,气候变化和人为活动对该地区长时间尺度(跨越一种以上气候状态)和广泛空间区域洪水发生的定量贡献尚不清楚。本研究旨在通过分析1961 - 2020年湄公河流域12个水文站的径流数据来解决这一问题。通过将峰值超过阈值(POT)方法与洪水事件开始和终止日的检测相结合,我们分析了两个不同时期的平均年洪水持续日数(MAFD)的变化:我们的研究结果表明,在整个研究期间,MLRYR的降水和洪水之间存在显著的正相关关系,尽管这种相关性在第二阶段比第一阶段弱。通过应用双质量曲线方法,我们将21世纪以来快速城市化时期与第一阶段进行比较,量化了气候变化和人为活动对MLRYR MAFD变化的贡献。城市化刚刚起步的时候。结果表明,人类活动显著抑制了二期平均年洪水发生率,贡献率在118% ~ 199%之间。相反,降水变化对第二期洪涝事件有正向影响,贡献率在18% ~ 99%之间。21世纪以来,大量的水利工程建设对黄河干支流径流的调节起到了至关重要的作用,从而削弱了黄河干支流的降水-洪水关系。这项研究表明,在未来的全球变暖和加速的城市化进程中,继续在湄公河流域建设水利工程可能仍然是缓解洪水风险增加的关键措施。
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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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