Analysis of regional river blocking by debris flows in response to climate change

被引:46
|
作者
Zou, Qiang [1 ,2 ]
Cui, Peng [1 ,2 ,4 ]
Jiang, Hu [1 ,3 ]
Wang, Jiao [1 ]
Li, Cong [1 ,4 ]
Zhou, Bin [1 ,4 ]
机构
[1] Chinese Acad Sci, Inst Mt Hazards & Environm IMHE, Key Lab Mt Hazards & Earth Surface Proc, Chengdu, Peoples R China
[2] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci CETES, Beijing, Peoples R China
[3] Southwest Univ Sci & Technol, Sch Environm & Resource, Mianyang, Sichuan, Peoples R China
[4] Univ Chinese Acad Sci, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
Debris flow; River blocking; Hazard analysis; Climate change; Dynamic environment; Qinghai-Tibet Plateau; RISK-ASSESSMENT; SEDIMENT; FLOOD; DAM; CONNECTIVITY; ENTRAINMENT; SIMULATION; PREDICTION; EVOLUTION; PHYSICS;
D O I
10.1016/j.scitotenv.2020.140262
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The river-blocking effects of debris flows have become common in numerous catchments in response to climate and environmental changes, and these effects have caused multiple, overlapping, and interconnected chain reactions that have led to huge losses in alpine regions. Considering this issue, this article developed a quantitative method for the regional river-blocking hazard assessment of debris flows by analyzing the in-depth relations among river-blocking hazard formation processes, factors and evolution mechanisms. Taking the debris flows in the Parlung Zangbo Basin in China as a case study, a multidimensional analysis was performed to analyze the characteristics of the hazard sequence and its relationship with climate change, including changes in temperature and precipitation. Accordingly, a new step toward a more comprehensive hazard assessment is proposed by establishing both a model and a system for regional river-blocking hazard assessment to analyze the debris flow evolution processes and environmental dynamics. Specifically, the sources of loose material were quantitatively estimated by establishing mathematical models based on the geometrical characteristics of diverse moraines, and the debris flow runoff was scientifically determined by focusing on the analysis of moraine sources, the brittleness index of the sediment mass and the geomorphological connectivity. Next, through coupling with the hydrodynamic conditions of debris flows and river flows, methods were established to determine the blocking degree of debris flow hazards at the regional scale. Validated by a field study and a remote-sensing interpretation of actual debris flows, a debris-flow induced river-blocking hazard map was obtained, and the assessment results were in accordance with the actual disaster situation. The analysis shows that the distribution of zones with high to very high levels of river blocking is closely correlated with the topographic characteristics and actual disaster sequences of debris flows. These findings suggest that the assessment results provide scientific support for engineering planning and hazard prevention in climate-sensitive areas; thus, the presented method may serve as pertinent guidance for regional river-blocking hazard assessments of debris flows in the Padung Zangbo Basin and beyond. (C) 2020 Elsevier B.V. All rights reserved.
引用
收藏
页数:16
相关论文
共 50 条
  • [31] Robust Climate Change Adaptation for Environmental Flows in the Goulburn River, Australia
    John, Andrew
    Horne, Avril
    Nathan, Rory
    Fowler, Keirnan
    Webb, J. Angus
    Stewardson, Michael
    FRONTIERS IN ENVIRONMENTAL SCIENCE, 2021, 9
  • [32] How might climate change affect river flows across the Thames Basin? An area-wide analysis using the UKCP09 Regional Climate Model ensemble
    Bell, V. A.
    Kay, A. L.
    Cole, S. J.
    Jones, R. G.
    Moore, R. J.
    Reynard, N. S.
    JOURNAL OF HYDROLOGY, 2012, 442 : 89 - 104
  • [33] Assessing the impacts of climate change on river flows in England using the UKCP09 climate change projections
    Charlton, Matthew B.
    Arnell, Nigel W.
    JOURNAL OF HYDROLOGY, 2014, 519 : 1723 - 1738
  • [34] Response of runoff to climate change in the Haihe River basin
    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing
    210029, China
    不详
    210029, China
    Shuikexue Jinzhan, 1 (1-9): : 1 - 9
  • [35] Centennial Channel Response to Climate Change in an Engineered River
    Arbos, C. Ylla
    Blom, A.
    Sloff, C. J.
    Schielen, R. M. J.
    GEOPHYSICAL RESEARCH LETTERS, 2023, 50 (08)
  • [36] Prolonged Response of River Terrace Flooding to Climate Change
    Vandenberghe, Jef
    Wang, Xianyan
    Yang, Xun
    QUATERNARY, 2024, 7 (02):
  • [37] Hydrological Response to Climate Change in the Weihe River Basin
    Cheng Lei
    Xu Zongxue
    Liu Zhaofei
    Yao Wenye
    PROCEEDINGS OF THE 4TH INTERNATIONAL YELLOW RIVER FORUM ON ECOLOGICAL CIVILIZATION AND RIVER ETHICS, VOL I, 2010, : 221 - +
  • [38] Response of Runoff to Climate Change in the Weihe River Basin
    Zuo Depeng
    Xu Zongxue
    PROCEEDINGS OF THE 5TH INTERNATIONAL YELLOW RIVER FORUM ON ENSURING WATER RIGHT OF THE RIVER'S DEMAND AND HEALTHY RIVER BASIN MAINTENANCE, VOL II, 2015, : 15 - 26
  • [39] Greenland Blocking Index 1851-2015: a regional climate change signal
    Hanna, Edward
    Cropper, Thomas E.
    Hall, Richard J.
    Cappelen, John
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2016, 36 (15) : 4847 - 4861
  • [40] Is the response of hill slope debris flows to recent climate change univocal? A case study in the Massif des Ecrins (French Alps)
    V. Jomelli
    D. Brunstein
    D. Grancher
    P. Pech
    Climatic Change, 2007, 85 : 119 - 137