State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China
Yuzhe Wang
College of Geography and Environment, Shandong Normal University, Jinan, 250014, China
Chuanxi Zhao
School of Water Conservancy and Environment, University of Jinan, Jinan, 250001, China
Qingyun Long
State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
Cunde Xiao
State Key Laboratory of Earth Surface Processes and Disaster Risk Reduction, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China
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EndNote: 207
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Total article views: 1,708 (including HTML, PDF, and XML)
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1,258
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1,708
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HTML: 1,258
PDF: 376
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BibTeX: 51
EndNote: 70
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2,303
480
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2,871
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HTML: 2,303
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Total: 2,871
BibTeX: 97
EndNote: 137
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Total article views: 4,579 (including HTML, PDF, and XML)
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Total article views: 1,708 (including HTML, PDF, and XML)
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Total article views: 2,871 (including HTML, PDF, and XML)
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This study investigates the 2018 Sedongpu glacier detachment in Southeastern Tibet using a two-dimensional ice flow model that includes an ice stiffness and basal slip positive feedback mechanism. The model simulates rapid transitions in glacier flow, triggering detachment when ice stress exceeds yield strength. The results, including ice speed and duration, align with observations, demonstrating the potential for early warning of similar hazards in the region.
This study investigates the 2018 Sedongpu glacier detachment in Southeastern Tibet using a...