Articles | Volume 17, issue 3
https://doi.org/10.5194/nhess-17-345-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/nhess-17-345-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Meteorological factors driving glacial till variation and the associated periglacial debris flows in Tianmo Valley, south-eastern Tibetan Plateau
Mingfeng Deng
Key Laboratory of Mountain Hazards and Surface Process, Institute
of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu
610041, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
Ningsheng Chen
CORRESPONDING AUTHOR
Key Laboratory of Mountain Hazards and Surface Process, Institute
of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu
610041, China
Mei Liu
Key Laboratory of Mountain Hazards and Surface Process, Institute
of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu
610041, China
College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 100049, China
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47 citations as recorded by crossref.
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47 citations as recorded by crossref.
- Analysis of regional river blocking by debris flows in response to climate change Q. Zou et al. 10.1016/j.scitotenv.2020.140262
- Dynamic process of a typical slope debris flow: a case study of the wujia gully, Zengda, Sichuan Province, China Y. Shunyu et al. 10.1007/s11069-021-05194-7
- A numerical model of debris flows with the Voellmy model over a real terrain J. Tang et al. 10.1007/s10346-022-01987-4
- Numerical investigation of debris flows using a two-phase continuum model incorporating a visco-inertial rheology Y. Xie et al. 10.1016/j.enggeo.2022.106797
- Initiation mechanisms and dynamics of a debris flow originated from debris-ice mixture slope failure in southeast Tibet, China D. Peng et al. 10.1016/j.enggeo.2022.106783
- Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier‐Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau J. Zhang et al. 10.1155/2022/3510944
- Debris flows originating in the mountain cryosphere under a changing climate: A review G. Yu et al. 10.1177/0309133320961705
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- Investigation of initiation conditions of periglacial debris flows in Sanggu watershed, Eastern Himalayas, Tibet Plateau (China) Z. Wang et al. 10.1007/s10346-022-02003-5
- Case Study: Effects of a Partial-Debris Dam on Riverbank Erosion in the Parlung Tsangpo River, China C. Choi et al. 10.3390/w10030250
- Novel Approach to Estimating Glacial Moraine Reserves in the Parlung Tsangpo Basin J. Wang et al. 10.3389/feart.2022.853089
- Susceptibility Analysis of Glacier Debris Flow by Investigating the Changes in Glaciers Based on Remote Sensing: A Case Study R. Lin et al. 10.3390/su13137196
- Hazard characteristics and causes of the “7.22” 2021 debris flow in Shenshuicao gully, Qilian Mountains, NW China Y. Yan et al. 10.1007/s10346-022-01992-7
- The grain size of sediments delivered to steep debris‐flow prone channels prior to and following wildfire A. Neely et al. 10.1002/esp.5819
- Debris flows originating from colluvium deposits in hollow regions during a heavy storm process in Taining, southeastern China Y. Zhang et al. 10.1007/s10346-019-01272-x
- Risk assessment of glacial debris flow on highway under warming climate: A case study of Tianmo Gully in the southeastern Tibetan Plateau Y. Li et al. 10.1016/j.ecolind.2024.112606
- Geohazard cascade and mechanism of large debris flows in Tianmo gully, SE Tibetan Plateau and implications to hazard monitoring R. Wei et al. 10.1016/j.enggeo.2017.12.013
- Prediction of the Periglacial Debris Flow in Southeast Tibet Based on Imbalanced Small Sample Data J. Du et al. 10.3390/w15020310
- Debris flow amplification in a moraine terrace and related engineering measures in the Zongzhai Valley, Southeastern Tibetan Plateau M. Deng et al. 10.1080/19475705.2018.1508507
- Damage Model and the Influence Factors of Mitigation Engineering against Glacial Debris Flow in the Parlung River Basin, SE Tibetan Plateau M. Lin et al. 10.3390/w15061098
- Hydromechanical coupling mechanism and an early warning method for paraglacial debris flows triggered by infiltration: Insights from field monitoring in Tianmo gully, Tibetan Plateau Z. Yang et al. 10.1007/s11069-023-05987-y
- A large-scale rock avalanche-debris flow cascading hazard in the Sedongpu catchment, southeastern Tibetan Plateau Y. Deng et al. 10.1007/s10346-024-02382-x
- Seismic and hydrological triggers for a complex cascading geohazard of the Tianmo Gully in the southeastern Tibetan Plateau R. Guo et al. 10.1016/j.enggeo.2023.107269
- High Mountain Asia hydropower systems threatened by climate-driven landscape instability D. Li et al. 10.1038/s41561-022-00953-y
- Mass flows and river response in rapid uplifting regions – A case of lower Yarlung Tsangpo basin, southeast Tibet, China G. Yu et al. 10.1016/j.ijsrc.2020.05.006
- Debris‐flow fan development and geomorphic effects in alpine canyons under a changing climate W. Hou & G. Yu 10.1002/esp.5699
- Effects of loose deposits on debris flow processes in the Aizi Valley, southwest China M. Liu et al. 10.1007/s11629-019-5388-9
- Geomorphic controls on debris flow activity in the paraglacial zone of the Southeast Tibetan Plateau J. Wang et al. 10.1007/s11069-023-05889-z
- New Insights into Ice Avalanche-Induced Debris Flows in Southeastern Tibet Using SAR Technology S. Luo et al. 10.3390/rs14112603
- Artificial Neural Network-based prediction of glacial debris flows in the ParlungZangbo Basin, southeastern Tibetan Plateau, China W. Tang et al. 10.1007/s11629-020-6414-7
- Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet K. Hu et al. 10.1038/s41598-021-95194-1
- Temperature and ice form effects on mechanical behaviors of ice-richmoraine soil of Tianmo valley nearby the Sichuan-Tibet Railway C. Li et al. 10.1016/j.enggeo.2022.106713
- Investigation of the triggering mechanism and runout characteristics of an earthflow in Zhimei village, Chengduo, Qinghai, China M. Zhang et al. 10.1007/s11069-021-04861-z
- Multi-Hazard Chain Reaction Initiated by the 2020 Meilong Debris Flow in the Dadu River, Southwest China L. Ning et al. 10.3389/feart.2022.827438
- Landscape change in response to multiperiod glacial debris flows in Peilong catchment, southeastern Tibet Z. Wang et al. 10.1007/s11629-020-6172-6
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- Prediction of debris flow blocking river hazard chain by the numerical simulation: the Cutou catchment, Wenchuan County, China X. Zhang et al. 10.1007/s10064-024-03588-y
- Analysis of the trigger conditions and activity trend in debris flow along Sichuan-Tibet traffic corridor (Xinduqiao-Changdu section) under environmental changes Y. Sun et al. 10.1007/s10064-024-03689-8
- A catastrophic landslide triggered debris flow in China’s Yigong: factors, dynamic processes, and tendency J. Li et al. 10.15446/esrj.v24n1.78094
- Faults and stratigraphic boundaries control evolution of the huge debris flows along the Jinjiang River, China Z. Liu et al. 10.3389/feart.2023.1237404
- Risk assessment of geological disasters in Nyingchi, Tibet C. Wu et al. 10.1515/geo-2020-0208
- Influence of freeze–thaw cycles on mechanical properties of moraine soils E. Qiu et al. 10.1016/j.trgeo.2023.101097
- Effects of water content on the shear behavior and critical state of glacial till in Tianmo Gully of Tibet, China G. Zhou et al. 10.1007/s11629-019-5440-9
- Disaster effects of climate change in High Mountain Asia: State of art and scientific challenges H. Wang et al. 10.1016/j.accre.2024.06.003
- Mechanical behaviour and grain breakage characteristics of Tibetan glacial tills under triaxial compression Z. Zeng et al. 10.1007/s11440-023-02195-7
Latest update: 13 Nov 2024
Short summary
Annual air temperature spiked and glacier retreated shortly before the three periglacial debris flows in Tianmo valley. However, they did not occur when glacier retreat was sharpest, resulting from the frozen bared glacial till as the melting of internal ice lags behind glacial retreat. The activity of the glacial till can be enhanced by prolonged high air temperature. Finally, either rainfall or continuous percolation of ice ablation water flows can generate debris flow.
Annual air temperature spiked and glacier retreated shortly before the three periglacial debris...
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