中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Accelerated River Meander Migration on the Tibetan Plateau Caused by Permafrost Thaw

文献类型:期刊论文

作者Sha, Anmeng11; Li, Dongfeng8,9,10,11; Walling, Des7; Zhao, Yi11; Tian, Shang11; Chen, Dong6; Deng, Shanshan5; Xia, Junqiang5; Best, Jim1,2,3,4
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2025-01-16
卷号52期号:1页码:12
关键词meander migration fluvial geomorphology climate change remote sensing permafrost degradation Tibetan Plateau
ISSN号0094-8276
DOI10.1029/2024GL111536
通讯作者Li, Dongfeng(dongfeng.li@pku.edu.cn)
英文摘要The migration of rivers in permafrost landscapes has critical implications for riverine infrastructure, ecosystem stability, and carbon cycling, yet its magnitude and underlying mechanisms remain poorly understood. Here, we leverage four decadal satellite imagery, hydrological observations, and permafrost modeling to investigate meander migration dynamics on the Tibetan Plateau. Our data show that the migration rates of permafrost rivers have increased by 34.6% from 1987 to 2022, in response to the combined effects of increased discharge, riverbank destabilization driven by ground ice melt and extended thawing days (increased by 35 days). In contrast, rivers flowing across seasonally frozen ground exhibited a decline in migration rate by 11.1%, driven by vegetation greening and riverbank stabilization. In a future warming climate for the Tibetan Plateau, the migration rates of permafrost rivers are anticipated to further accelerate, potentially threatening riverine infrastructure safety and aquatic ecosystems, and intensifying the permafrost carbon cycle.
资助项目National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities, Peking University[7100604495] ; Excellent Young Scientists Fund of the National Natural Science Foundation of China ; [52479055] ; [92047303]
WOS研究方向Geology
语种英语
WOS记录号WOS:001389831600001
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities, Peking University ; Excellent Young Scientists Fund of the National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/212435]  
专题中国科学院地理科学与资源研究所
通讯作者Li, Dongfeng
作者单位1.Univ Illinois, Dept Geog & GIS, Urbana, IL USA
2.Univ Illinois, Ven Chow Hydrosyst Lab, Urbana, IL USA
3.Univ Illinois, Dept Mech Sci & Engn, Urbana, IL USA
4.Univ Illinois, Dept Earth Sci & Environm Change, Urbana, IL USA
5.Wuhan Univ, State Key Lab Water Resources & Hydropower Engn Sc, Wuhan, Peoples R China
6.Chinese Acad Sci, Key Lab Water Cycle & Related Land Surface Proc, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China
7.Univ Exeter, Dept Geog, Fac Environm Sci & Econ, Exeter, England
8.Peking Univ, Inst Carbon Neutral, Beijing, Peoples R China
9.Peking Univ, Inst Tibetan Plateau, Beijing, Peoples R China
10.Peking Univ, State Environm Protect Key Lab All Mat Flux River, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Sha, Anmeng,Li, Dongfeng,Walling, Des,et al. Accelerated River Meander Migration on the Tibetan Plateau Caused by Permafrost Thaw[J]. GEOPHYSICAL RESEARCH LETTERS,2025,52(1):12.
APA Sha, Anmeng.,Li, Dongfeng.,Walling, Des.,Zhao, Yi.,Tian, Shang.,...&Best, Jim.(2025).Accelerated River Meander Migration on the Tibetan Plateau Caused by Permafrost Thaw.GEOPHYSICAL RESEARCH LETTERS,52(1),12.
MLA Sha, Anmeng,et al."Accelerated River Meander Migration on the Tibetan Plateau Caused by Permafrost Thaw".GEOPHYSICAL RESEARCH LETTERS 52.1(2025):12.

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来源:地理科学与资源研究所

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