Articles | Volume 11, issue 1
https://doi.org/10.5194/essd-11-35-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-11-35-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Two multi-temporal datasets that track the enhanced landsliding after the 2008 Wenchuan earthquake
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
Gianvito Scaringi
Institute of Hydrogeology, Engineering Geology and Applied Geophysics, Faculty of Science, Charles University, Prague, 128 43, Czech Republic
Guillem Domènech
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
Key Laboratory of Mountain Hazards and Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610041, China
Lanxin Dai
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
Chaoyang He
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
Qiang Xu
CORRESPONDING AUTHOR
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
Runqiu Huang
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu, 610059, China
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- Probabilistic identification of debris flow source areas in the Wenchuan earthquake-affected region of China based on Bayesian geomorphology X. Hu et al. 10.1007/s12665-024-11833-6
- Investigation of the 2019 Wenchuan County debris flow disaster suggests nonuniform spatial and temporal post-seismic debris flow evolution patterns X. Zhang et al. 10.1007/s10346-022-01896-6
- A thermo-hydro-mechanical approach to soil slope stability under climate change G. Scaringi & M. Loche 10.1016/j.geomorph.2022.108108
- Identifying the Characteristics and Implications of Post-Earthquake Debris Flow Events Based on Multi-Source Remote Sensing Images W. Jin et al. 10.3390/rs16173336
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- Analysing post-earthquake landslide susceptibility using multi-temporal landslide inventories — a case study in Miansi Town of China N. Li et al. 10.1007/s11629-019-5681-7
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- Estimating the debris-flow magnitude using landslide sediment connectivity, Qipan catchment, Wenchuan County, China X. Hu et al. 10.1016/j.catena.2022.106689
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 04 Nov 2024
Short summary
Large earthquakes cause major disturbances to mountain landscapes. They trigger many landslides that can form deposits of debris on steep slopes and channels. Rainfall can remobilise these deposits and generate large and destructive flow-like landslides and floods. We release two datasets that track a decade of landsliding following the 2008 7.9 magnitude Wenchuan earthquake in China. These data are useful for quantifying the role of major earthquakes in shaping mountain landscapes.
Large earthquakes cause major disturbances to mountain landscapes. They trigger many landslides...
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Final-revised paper
Preprint