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作 者:Guangyao Gao Anqi Huang Lishan Ran Dongfeng Li Hong Zhang Yadu Pokhrel Liqiang Yao Bojie Fu 高光耀;黄安琪;冉立山;李东锋;张洪;Yadu Pokhrel;姚立强;傅伯杰
机构地区:[1]State Key Laboratory of Urban and Regional Ecology,Research Center for Eco-Environmental Sciences,Chinese Academy of Sciences,Beijing 100085,China [2]State Key Laboratory of Environmental Aquatic Chemistry,Research Center for Eco-Environmental Sciences,Chinese Academy of Sciences,Beijing 100085,China [3]University of Chinese Academy of Sciences,Beijing 100049,China [4]Department of Geography,The University of Hong Kong,Hong Kong 999077,China [5]Key Laboratory for Water and Sediment Sciences,Ministry of Education,College of Environmental Sciences and Engineering,Peking University,Beijing 100871,China [6]Department of Civil and Environmental Engineering,Michigan State University,East Lansing MI 48824,USA [7]Water Resources Department,Yangtze River Scientific Research Institute,Wuhan 430010,China
出 处:《Science Bulletin》2025年第6期866-870,共5页科学通报(英文版)
基 金:supported by the National Key Research and Development Program of China(2017YFA0604703);the National Natural Science Foundation of China(42041004);the Youth Innovation Promotion Association of Chinese Academic Sciences(Y202013).
摘 要:Streamflow and sediment transport in river ecosystems are crit-ical processes for material movement and energy conversion,intri-cately linked to socioeconomic and riverine biophysical processes such as hydropower development,flood mitigation,reservoir silta-tion,and channel adjustment[1].Streamflow-sediment load(Q-S)relationships are fundamental to improving the assessment and prediction of these riverine processes and flux patterns.Damming has substantially regulated large river systems,leading to a signif-icant decreasing trend in both streamflow and sediment load,resulting in far-reaching impacts on water quality and ecological stability[2].In the context of intensifying hydrological extremes.
关 键 词:prediction Yangtze River Basin extreme streamflow hydropower developmentflood mitigationreservoir sediment relationships channel adjustment streamflow sediment dam regulation streamflow sediment transport
分 类 号:TV14[水利工程—水力学及河流动力学]
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