Articles | Volume 21, issue 10
https://doi.org/10.5194/nhess-21-3015-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-21-3015-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Oct 2021
Research article |
| 08 Oct 2021
| 08 Oct 2021
Debris flow event on Osorno volcano, Chile, during summer 2017: new interpretations for chain processes in the southern Andes
Ivo Janos Fustos-Toribio
CORRESPONDING AUTHOR
Department of Civil Engineering, University of La Frontera,
Francisco Salazar 1145, Temuco, Chile
Bastian Morales-Vargas
Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Department of Forest Sciences, Faculty of Agriculture and Forest
Sciences, Universidad de La Frontera, Av. Francisco Salazar 01145, Temuco,
4780000, Chile
Marcelo Somos-Valenzuela
CORRESPONDING AUTHOR
Department of Forest Sciences, Faculty of Agriculture and Forest
Sciences, Universidad de La Frontera, Av. Francisco Salazar 01145, Temuco,
4780000, Chile
Butamallín Research Center for Global Change, University of La
Frontera, Av. Francisco Salazar 01145, Temuco, 4780000, Chile
Pablo Moreno-Yaeger
Department of Civil Engineering, University of La Frontera,
Francisco Salazar 1145, Temuco, Chile
Department of Geoscience, University of Wisconsin–Madison, 1215
West Dayton St., Madison, WI 53706, USA
Ramiro Muñoz-Ramirez
Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Ines Rodriguez Araneda
Departamento de Obras Civiles y Geología, Facultad de
Ingeniería, Universidad Católica de Temuco, Rudecindo Ortega 02950,
Temuco, Chile
Ningsheng Chen
Key Laboratory of Mountain Hazards and Surface Processes, Institute
of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu
610041, China
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Nat. Hazards Earth Syst. Sci., 22, 2169–2183, https://doi.org/10.5194/nhess-22-2169-2022, https://doi.org/10.5194/nhess-22-2169-2022, 2022
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We develop for the first time a rainfall-induced landslide early warning system for the south of Chile. We used forecast precipitation values at different scales using mesoscale models to evaluate the probability of landslides using statistical models. We showed the feasibility of implementing these models in future, supporting stakeholders and decision-makers.
Marcelo A. Somos-Valenzuela, Joaquín E. Oyarzún-Ulloa, Ivo J. Fustos-Toribio, Natalia Garrido-Urzua, and Ningsheng Chen
Nat. Hazards Earth Syst. Sci., 20, 2319–2333, https://doi.org/10.5194/nhess-20-2319-2020, https://doi.org/10.5194/nhess-20-2319-2020, 2020
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This work presents a study of the biggest mudflow event in 20 years in Chilean Patagonia, which resulted from an avalanche in the Cordon Yelcho. We integrate in situ geotechnical tests and numerical modeling to model the Villa Santa Lucía mudflow event. Our results suggest that the initial soil water content is sufficient to transform the landslide and scoured soil into a mudflow. Therefore, knowing the soil characteristics is crucial to evaluating the impact of landslides in the study area.
Bastian Morales, Marcelo Somos-Valenzuela, Mario Lillo, Iñigo Irarrazaval, David Farias, Elizabet Lizama, Diego Rivera, and Alfonso Fernández
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Through a physical model, we explored how lacier geometry and topography configuration constrains glacier thinning in the Patagonian Icefields, the world's main glacial freshwater reservoir after Antarctica and Greenland. Our results indicate that about 53 % of the Patagonian Icefield ice flow is susceptible to thinning. Our findings allow for identifying priority glaciers for future research considering climate change projections.
Alton C. Byers, Marcelo Somos-Valenzuela, Dan H. Shugar, Daniel McGrath, Mohan B. Chand, and Ram Avtar
The Cryosphere, 18, 711–717, https://doi.org/10.5194/tc-18-711-2024, https://doi.org/10.5194/tc-18-711-2024, 2024
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In spite of enhanced technologies, many large cryospheric events remain unreported because of their remoteness, inaccessibility, or poor communications. In this Brief communication, we report on a large ice-debris avalanche that occurred sometime between 16 and 21 August 2022 in the Kanchenjunga Conservation Area (KCA), eastern Nepal.
Ivo Fustos-Toribio, Nataly Manque-Roa, Daniel Vásquez Antipan, Mauricio Hermosilla Sotomayor, and Viviana Letelier Gonzalez
Nat. Hazards Earth Syst. Sci., 22, 2169–2183, https://doi.org/10.5194/nhess-22-2169-2022, https://doi.org/10.5194/nhess-22-2169-2022, 2022
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We develop for the first time a rainfall-induced landslide early warning system for the south of Chile. We used forecast precipitation values at different scales using mesoscale models to evaluate the probability of landslides using statistical models. We showed the feasibility of implementing these models in future, supporting stakeholders and decision-makers.
Marcelo A. Somos-Valenzuela, Joaquín E. Oyarzún-Ulloa, Ivo J. Fustos-Toribio, Natalia Garrido-Urzua, and Ningsheng Chen
Nat. Hazards Earth Syst. Sci., 20, 2319–2333, https://doi.org/10.5194/nhess-20-2319-2020, https://doi.org/10.5194/nhess-20-2319-2020, 2020
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This work presents a study of the biggest mudflow event in 20 years in Chilean Patagonia, which resulted from an avalanche in the Cordon Yelcho. We integrate in situ geotechnical tests and numerical modeling to model the Villa Santa Lucía mudflow event. Our results suggest that the initial soil water content is sufficient to transform the landslide and scoured soil into a mudflow. Therefore, knowing the soil characteristics is crucial to evaluating the impact of landslides in the study area.
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This study assesses the usability of WRF model-simulated soil moisture for landslide monitoring in northern Italy. In particular, three advanced land surface model schemes (Noah, Noah-MP, and CLM4) are used to provide multi-layer soil moisture data. The results have shown Noah-MP can provide the best landslide monitoring performance. It is also demonstrated that a single soil moisture sensor located in plain area has a high correlation with a significant proportion of the study area.
Alvaro Hofflinger, Marcelo A. Somos-Valenzuela, and Arturo Vallejos-Romero
Nat. Hazards Earth Syst. Sci., 19, 251–267, https://doi.org/10.5194/nhess-19-251-2019, https://doi.org/10.5194/nhess-19-251-2019, 2019
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In this work, we propose a novel methodology (ReTSVI) to integrate a social vulnerability index into flood hazard methodologies. ReTSVI combines a series of modules that are pieces of information that interact during an evacuation, such as evacuation rate curves, mobilization, inundation models, and social vulnerability indexes, to create an integrated map of the evacuation rate in a given location.
Mingfeng Deng, Yong Zhang, Mei Liu, Yuanhuan Wang, Wanyin Xie, and Ningsheng Chen
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2017-390, https://doi.org/10.5194/nhess-2017-390, 2017
Preprint withdrawn
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Research of the post-wildfire in Reneyong Valley shows: (1) the thresholds of post-fire debris flows was low and tend to increase as time passes; (2) reason for the post-fire debris flows with high frequency lies in an increase in soil water repellency, the soft geology, drainage area, channel gradient and regional arid climate; and (3) the varied rainfall thresholds (low in branch No. 3 and higher in branch No. 1 and No. 2) among the different branches are dependent on the drainage area.
Mingfeng Deng, Ningsheng Chen, and Mei Liu
Nat. Hazards Earth Syst. Sci., 17, 345–356, https://doi.org/10.5194/nhess-17-345-2017, https://doi.org/10.5194/nhess-17-345-2017, 2017
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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.
N. Sh. Chen, G. Sh. Hu, W. Deng, N. Khanal, Y. H. Zhu, and D. Han
Nat. Hazards Earth Syst. Sci., 13, 795–808, https://doi.org/10.5194/nhess-13-795-2013, https://doi.org/10.5194/nhess-13-795-2013, 2013
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Shallow-landslide stability evaluation in loess areas according to the Revised Infinite Slope Model: a case study of the 7.25 Tianshui sliding-flow landslide events of 2013 in the southwest of the Loess Plateau, China
Probabilistic assessment of postfire debris-flow inundation in response to forecast rainfall
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Francis K. Rengers, Samuel Bower, Andrew Knapp, Jason W. Kean, Danielle W. vonLembke, Matthew A. Thomas, Jaime Kostelnik, Katherine R. Barnhart, Matthew Bethel, Joseph E. Gartner, Madeline Hille, Dennis M. Staley, Justin K. Anderson, Elizabeth K. Roberts, Stephen B. DeLong, Belize Lane, Paxton Ridgway, and Brendan P. Murphy
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Praveen Kumar, Priyanka Priyanka, Kala Venkata Uday, and Varun Dutt
Nat. Hazards Earth Syst. Sci., 24, 1913–1928, https://doi.org/10.5194/nhess-24-1913-2024, https://doi.org/10.5194/nhess-24-1913-2024, 2024
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Kristian Svennevig, Julian Koch, Marie Keiding, and Gregor Luetzenburg
Nat. Hazards Earth Syst. Sci., 24, 1897–1911, https://doi.org/10.5194/nhess-24-1897-2024, https://doi.org/10.5194/nhess-24-1897-2024, 2024
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In our study, we analysed publicly available data in order to investigate the impact of climate change on landslides in Denmark. Our research indicates that the rising groundwater table due to climate change will result in an increase in landslide activity. Previous incidents of extremely wet winters have caused damage to infrastructure and buildings due to landslides. This study is the first of its kind to exclusively rely on public data and examine landslides in Denmark.
Jiao Wang, Zhangxing Wang, Guanhua Sun, and Hongming Luo
Nat. Hazards Earth Syst. Sci., 24, 1741–1756, https://doi.org/10.5194/nhess-24-1741-2024, https://doi.org/10.5194/nhess-24-1741-2024, 2024
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With a simplified formula linking rainfall and groundwater level, the rise of the phreatic surface within the slope can be obtained. Then, a global analysis method that considers both seepage and seismic forces is proposed to determine the safety factor of slopes subjected to the combined effect of rainfall and earthquakes. By taking a slope in the Three Gorges Reservoir area as an example, the safety evolution of the slope combined with both rainfall and earthquake is also examined.
Carlo Tacconi Stefanelli, William Frodella, Francesco Caleca, Zhanar Raimbekova, Ruslan Umaraliev, and Veronica Tofani
Nat. Hazards Earth Syst. Sci., 24, 1697–1720, https://doi.org/10.5194/nhess-24-1697-2024, https://doi.org/10.5194/nhess-24-1697-2024, 2024
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Central Asia regions are marked by active tectonics, high mountains with glaciers, and strong rainfall. These predisposing factors make large landslides a serious threat in the area and a source of possible damming scenarios, which endanger the population. To prevent this, a semi-automated geographic information system (GIS-)based mapping method, centered on a bivariate correlation of morphometric parameters, was applied to give preliminary information on damming susceptibility in Central Asia.
Rex L. Baum, Dianne L. Brien, Mark E. Reid, William H. Schulz, and Matthew J. Tello
Nat. Hazards Earth Syst. Sci., 24, 1579–1605, https://doi.org/10.5194/nhess-24-1579-2024, https://doi.org/10.5194/nhess-24-1579-2024, 2024
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We mapped potential for heavy rainfall to cause landslides in part of the central mountains of Puerto Rico using new tools for estimating soil depth and quasi-3D slope stability. Potential ground-failure locations correlate well with the spatial density of landslides from Hurricane Maria. The smooth boundaries of the very high and high ground-failure susceptibility zones enclose 75 % and 90 %, respectively, of observed landslides. The maps can help mitigate ground-failure hazards.
Katherine R. Barnhart, Christopher R. Miller, Francis K. Rengers, and Jason W. Kean
Nat. Hazards Earth Syst. Sci., 24, 1459–1483, https://doi.org/10.5194/nhess-24-1459-2024, https://doi.org/10.5194/nhess-24-1459-2024, 2024
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Debris flows are a type of fast-moving landslide that start from shallow landslides or during intense rain. Infrastructure located downstream of watersheds susceptible to debris flows may be damaged should a debris flow reach them. We present and evaluate an approach to forecast building damage caused by debris flows. We test three alternative models for simulating the motion of debris flows and find that only one can forecast the correct number and spatial pattern of damaged buildings.
Luke A. McGuire, Francis K. Rengers, Ann M. Youberg, Alexander N. Gorr, Olivia J. Hoch, Rebecca Beers, and Ryan Porter
Nat. Hazards Earth Syst. Sci., 24, 1357–1379, https://doi.org/10.5194/nhess-24-1357-2024, https://doi.org/10.5194/nhess-24-1357-2024, 2024
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Runoff and erosion increase after fire, leading to a greater likelihood of floods and debris flows. We monitored debris flow activity following a fire in western New Mexico, USA, and observed 16 debris flows over a <2-year monitoring period. Rainstorms with recurrence intervals of approximately 1 year were sufficient to initiate debris flows. All debris flows initiated during the first several months following the fire, indicating a rapid decrease in debris flow susceptibility over time.
Oliver Korup, Lisa Luna, and Joaquin Ferrer
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2024-55, https://doi.org/10.5194/nhess-2024-55, 2024
Revised manuscript accepted for NHESS
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Catalogues of mapped landslides are useful for learning and forecasting how frequently they occur in relation to their size. Yet, rare and large landslides remain most uncertain in statistical summaries of these catalogues. We propose a single, consistent method of comparing across different data sources, and find that landslide statistics disclose more about subjective mapping choices than trigger types or environmental setting.
Ken'ichi Koshimizu, Satoshi Ishimaru, Fumitoshi Imaizumi, and Gentaro Kawakami
Nat. Hazards Earth Syst. Sci., 24, 1287–1301, https://doi.org/10.5194/nhess-24-1287-2024, https://doi.org/10.5194/nhess-24-1287-2024, 2024
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Morphological conditions of drainage basins that classify the presence or absence of debris flow fans were analyzed in areas with different rock strength using decision tree analysis. The relief ratio is the most important morphological factor regardless of the geology. However, the thresholds of morphological parameters needed for forming debris flow fans differ depending on the geology. Decision tree analysis is an effective tool for evaluating the debris flow risk for each geology.
Daniel Bolliger, Fritz Schlunegger, and Brian W. McArdell
Nat. Hazards Earth Syst. Sci., 24, 1035–1049, https://doi.org/10.5194/nhess-24-1035-2024, https://doi.org/10.5194/nhess-24-1035-2024, 2024
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We analysed data from the Illgraben debris flow monitoring station, Switzerland, and we modelled these flows with a debris flow runout model. We found that no correlation exists between the grain size distribution, the mineralogical composition of the matrix, and the debris flow properties. The flow properties rather appear to be determined by the flow volume, from which most other parameters can be derived.
Yuntao Zhou, Xiaoyan Zhao, Guangze Zhang, Bernd Wünnemann, Jiajia Zhang, and Minghui Meng
Nat. Hazards Earth Syst. Sci., 24, 891–906, https://doi.org/10.5194/nhess-24-891-2024, https://doi.org/10.5194/nhess-24-891-2024, 2024
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We developed three rock bridge models to analyze 3D stability and deformation behaviors of the Tizicao landslide and found that the contact surface model with high strength parameters combines advantages of the intact rock mass model in simulating the deformation of slopes with rock bridges and the modeling advantage of the Jennings model. The results help in choosing a rock bridge model to simulate landslide stability and reveal the influence laws of rock bridges on the stability of landslides.
Ashok Dahal, Hakan Tanyas, Cees van Westen, Mark van der Meijde, Paul Martin Mai, Raphaël Huser, and Luigi Lombardo
Nat. Hazards Earth Syst. Sci., 24, 823–845, https://doi.org/10.5194/nhess-24-823-2024, https://doi.org/10.5194/nhess-24-823-2024, 2024
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We propose a modeling approach capable of recognizing slopes that may generate landslides, as well as how large these mass movements may be. This protocol is implemented, tested, and validated with data that change in both space and time via an Ensemble Neural Network architecture.
Li-Ru Luo, Zhi-Xiang Yu, Li-Jun Zhang, Qi Wang, Lin-Xu Liao, and Li Peng
Nat. Hazards Earth Syst. Sci., 24, 631–649, https://doi.org/10.5194/nhess-24-631-2024, https://doi.org/10.5194/nhess-24-631-2024, 2024
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We performed field investigations on a rockfall near Jiguanshan National Forest Park, Chengdu. Vital information was obtained from an unmanned aerial vehicle survey. A finite element model was created to reproduce the damage evolution. We found that the impact kinetic energy was below the design protection energy. Improper member connections prevent the barrier from producing significant deformation to absorb energy. Damage is avoided by improving the ability of the nets and ropes to slide.
Rachael Lau, Carolina Seguí, Tyler Waterman, Nathaniel Chaney, and Manolis Veveakis
EGUsphere, https://doi.org/10.48550/arXiv.2311.01564, https://doi.org/10.48550/arXiv.2311.01564, 2024
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This work examines the use of Interferometric Synthetic Aperture Radar (InSAR) alongside in-situ borehole measurements to assess the stability of deep-seated landslides for the case study of El Forn (Andorra). InSAR data compared with borehole data suggests a key tradeoff between accuracy and precision for various InSAR resolutions. Spatial interpolation with InSAR informed how many remote observations are necessary to lower error on remote-sensing recreation of ground motion over the landslide.
Sudhanshu Dixit, Srikrishnan Siva Subramanian, Piyush Srivastava, Ali P. Yunus, Tapas Ranjan Martha, and Sumit Sen
Nat. Hazards Earth Syst. Sci., 24, 465–480, https://doi.org/10.5194/nhess-24-465-2024, https://doi.org/10.5194/nhess-24-465-2024, 2024
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Rainfall intensity–duration (ID) thresholds can aid in the prediction of natural hazards. Large-scale sediment disasters like landslides, debris flows, and flash floods happen frequently in the Himalayas because of their propensity for intense precipitation events. We provide a new framework that combines the Weather Research and Forecasting (WRF) model with a regionally distributed numerical model for debris flows to analyse and predict intense rainfall-induced landslides in the Himalayas.
Jacob B. Woodard, Benjamin B. Mirus, Nathan J. Wood, Kate E. Allstadt, Benjamin A. Leshchinsky, and Matthew M. Crawford
Nat. Hazards Earth Syst. Sci., 24, 1–12, https://doi.org/10.5194/nhess-24-1-2024, https://doi.org/10.5194/nhess-24-1-2024, 2024
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Dividing landscapes into hillslopes greatly improves predictions of landslide potential across landscapes, but their scaling is often arbitrarily set and can require significant computing power to delineate. Here, we present a new computer program that can efficiently divide landscapes into meaningful slope units scaled to best capture landslide processes. The results of this work will allow an improved understanding of landslide potential and can help reduce the impacts of landslides worldwide.
Anne Felsberg, Zdenko Heyvaert, Jean Poesen, Thomas Stanley, and Gabriëlle J. M. De Lannoy
Nat. Hazards Earth Syst. Sci., 23, 3805–3821, https://doi.org/10.5194/nhess-23-3805-2023, https://doi.org/10.5194/nhess-23-3805-2023, 2023
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The Probabilistic Hydrological Estimation of LandSlides (PHELS) model combines ensembles of landslide susceptibility and of hydrological predictor variables to provide daily, global ensembles of hazard for hydrologically triggered landslides. Testing different hydrological predictors showed that the combination of rainfall and soil moisture performed best, with the lowest number of missed and false alarms. The ensemble approach allowed the estimation of the associated prediction uncertainty.
Xushan Shi, Bo Chai, Juan Du, Wei Wang, and Bo Liu
Nat. Hazards Earth Syst. Sci., 23, 3425–3443, https://doi.org/10.5194/nhess-23-3425-2023, https://doi.org/10.5194/nhess-23-3425-2023, 2023
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A 3D stability analysis method is proposed for biased rockfall with external erosion. Four failure modes are considered according to rockfall evolution processes, including partial damage of underlying soft rock and overall failure of hard rock blocks. This method is validated with the biased rockfalls in the Sichuan Basin, China. The critical retreat ratio from low to moderate rockfall susceptibility is 0.33. This method could facilitate rockfall early identification and risk mitigation.
Zhen Lei Wei, Yue Quan Shang, Qiu Hua Liang, and Xi Lin Xia
Nat. Hazards Earth Syst. Sci. Discuss., https://doi.org/10.5194/nhess-2023-180, https://doi.org/10.5194/nhess-2023-180, 2023
Revised manuscript accepted for NHESS
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The initiation of debris flows is influenced significantly by rainfall-induced hydrological processes. We propose a novel framework, which is based on an integrated hydrological and hydrodynamic model, aimed at estimating Intensity-Duration (I-D) rainfall thresholds responsible for triggering debris flows. In comparison to traditional statistical approaches, this physically-based framework particularly suitable for application in ungauged catchments where historical debris flow data is scarce.
Marius Schneider, Nicolas Oestreicher, Thomas Ehrat, and Simon Loew
Nat. Hazards Earth Syst. Sci., 23, 3337–3354, https://doi.org/10.5194/nhess-23-3337-2023, https://doi.org/10.5194/nhess-23-3337-2023, 2023
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Rockfalls and their hazards are typically treated as statistical events based on rockfall catalogs, but only a few complete rockfall inventories are available today. Here, we present new results from a Doppler radar rockfall alarm system, which has operated since 2018 at a high frequency under all illumination and weather conditions at a site where frequent rockfall events threaten a village and road. The new data set is used to investigate rockfall triggers in an active rockslide complex.
Jürgen Mey, Ravi Kumar Guntu, Alexander Plakias, Igo Silva de Almeida, and Wolfgang Schwanghart
EGUsphere, https://doi.org/10.5194/egusphere-2023-1975, https://doi.org/10.5194/egusphere-2023-1975, 2023
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The Himalayan road network links remote areas, but fragile terrain and poor construction lead to frequent landslides. This study on NH-7 in India's Uttarakhand region analyzed 300 landslides after heavy 2022 rainfall. Factors like slope, rainfall, rock type, and road work influence landslides. The study's model predicts landslide locations for better road maintenance planning, highlighting the risk from climate change and increased road use.
Annette I. Patton, Lisa V. Luna, Joshua J. Roering, Aaron Jacobs, Oliver Korup, and Benjamin B. Mirus
Nat. Hazards Earth Syst. Sci., 23, 3261–3284, https://doi.org/10.5194/nhess-23-3261-2023, https://doi.org/10.5194/nhess-23-3261-2023, 2023
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Landslide warning systems often use statistical models to predict landslides based on rainfall. They are typically trained on large datasets with many landslide occurrences, but in rural areas large datasets may not exist. In this study, we evaluate which statistical model types are best suited to predicting landslides and demonstrate that even a small landslide inventory (five storms) can be used to train useful models for landslide early warning when non-landslide events are also included.
Sandra Melzner, Marco Conedera, Johannes Hübl, and Mauro Rossi
Nat. Hazards Earth Syst. Sci., 23, 3079–3093, https://doi.org/10.5194/nhess-23-3079-2023, https://doi.org/10.5194/nhess-23-3079-2023, 2023
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The estimation of the temporal frequency of the involved rockfall processes is an important part in hazard and risk assessments. Different methods can be used to collect and analyse rockfall data. From a statistical point of view, rockfall datasets are nearly always incomplete. Accurate data collection approaches and the application of statistical methods on existing rockfall data series as reported in this study should be better considered in rockfall hazard and risk assessments in the future.
Stefan Hergarten
Nat. Hazards Earth Syst. Sci., 23, 3051–3063, https://doi.org/10.5194/nhess-23-3051-2023, https://doi.org/10.5194/nhess-23-3051-2023, 2023
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Rockslides are a major hazard in mountainous regions. In formerly glaciated regions, the disposition mainly arises from oversteepened topography and decreases through time. However, little is known about this decrease and thus about the present-day hazard of huge, potentially catastrophic rockslides. This paper presents a new theoretical framework that explains the decrease in maximum rockslide size through time and predicts the present-day frequency of large rockslides for the European Alps.
Colin K. Bloom, Corinne Singeisen, Timothy Stahl, Andrew Howell, Chris Massey, and Dougal Mason
Nat. Hazards Earth Syst. Sci., 23, 2987–3013, https://doi.org/10.5194/nhess-23-2987-2023, https://doi.org/10.5194/nhess-23-2987-2023, 2023
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Landslides are often observed on coastlines following large earthquakes, but few studies have explored this occurrence. Here, statistical modelling of landslides triggered by the 2016 Kaikōura earthquake in New Zealand is used to investigate factors driving coastal earthquake-induced landslides. Geology, steep slopes, and shaking intensity are good predictors of landslides from the Kaikōura event. Steeper slopes close to the coast provide the best explanation for a high landslide density.
Yi-Min Huang
Nat. Hazards Earth Syst. Sci., 23, 2649–2662, https://doi.org/10.5194/nhess-23-2649-2023, https://doi.org/10.5194/nhess-23-2649-2023, 2023
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Debris flows are common hazards in Taiwan, and debris-flow early warning is important for disaster responses. The rainfall thresholds of debris flows are analyzed and determined in terms of rainfall intensity, accumulated rainfall, and rainfall duration, based on case histories in Taiwan. These thresholds are useful for disaster management, and the cases in Taiwan are useful for global debris-flow databases.
Davide Notti, Martina Cignetti, Danilo Godone, and Daniele Giordan
Nat. Hazards Earth Syst. Sci., 23, 2625–2648, https://doi.org/10.5194/nhess-23-2625-2023, https://doi.org/10.5194/nhess-23-2625-2023, 2023
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We developed a cost-effective and user-friendly approach to map shallow landslides using free satellite data. Our methodology involves analysing the pre- and post-event NDVI variation to semi-automatically detect areas potentially affected by shallow landslides (PLs). Additionally, we have created Google Earth Engine scripts to rapidly compute NDVI differences and time series of affected areas. Datasets and codes are stored in an open data repository for improvement by the scientific community.
Simon Seelig, Thomas Wagner, Karl Krainer, Michael Avian, Marc Olefs, Klaus Haslinger, and Gerfried Winkler
Nat. Hazards Earth Syst. Sci., 23, 2547–2568, https://doi.org/10.5194/nhess-23-2547-2023, https://doi.org/10.5194/nhess-23-2547-2023, 2023
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A rapid sequence of cascading events involving thermokarst lake outburst, rock glacier front failure, debris flow development, and river blockage hit an alpine valley in Austria during summer 2019. We analyze the environmental conditions initiating the process chain and identify the rapid evolution of a thermokarst channel network as the main driver. Our results highlight the need to account for permafrost degradation in debris flow hazard assessment studies.
Camilla Lanfranconi, Paolo Frattini, Gianluca Sala, Giuseppe Dattola, Davide Bertolo, Juanjuan Sun, and Giovanni Battista Crosta
Nat. Hazards Earth Syst. Sci., 23, 2349–2363, https://doi.org/10.5194/nhess-23-2349-2023, https://doi.org/10.5194/nhess-23-2349-2023, 2023
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This paper presents a study on rockfall dynamics and hazard, examining the impact of the presence of trees along slope and block fragmentation. We compared rockfall simulations that explicitly model the presence of trees and fragmentation with a classical approach that accounts for these phenomena in model parameters (both the hazard and the kinetic energy change). We also used a non-parametric probabilistic rockfall hazard analysis method for hazard mapping.
Ascanio Rosi, William Frodella, Nicola Nocentini, Francesco Caleca, Hans Balder Havenith, Alexander Strom, Mirzo Saidov, Gany Amirgalievich Bimurzaev, and Veronica Tofani
Nat. Hazards Earth Syst. Sci., 23, 2229–2250, https://doi.org/10.5194/nhess-23-2229-2023, https://doi.org/10.5194/nhess-23-2229-2023, 2023
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This work was carried out within the Strengthening Financial Resilience and Accelerating Risk Reduction in Central Asia (SFRARR) project and is focused on the first landslide susceptibility analysis at a regional scale for Central Asia. The most detailed available landslide inventories were implemented in a random forest model. The final aim was to provide a useful tool for reduction strategies to landslide scientists, practitioners, and administrators.
Francis K. Rengers, Luke A. McGuire, Katherine R. Barnhart, Ann M. Youberg, Daniel Cadol, Alexander N. Gorr, Olivia J. Hoch, Rebecca Beers, and Jason W. Kean
Nat. Hazards Earth Syst. Sci., 23, 2075–2088, https://doi.org/10.5194/nhess-23-2075-2023, https://doi.org/10.5194/nhess-23-2075-2023, 2023
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Debris flows often occur after wildfires. These debris flows move water, sediment, and wood. The wood can get stuck in channels, creating a dam that holds boulders, cobbles, sand, and muddy material. We investigated how the channel width and wood length influenced how much sediment is stored. We also used a series of equations to back calculate the debris flow speed using the breaking threshold of wood. These data will help improve models and provide insight into future field investigations.
Maxime Morel, Guillaume Piton, Damien Kuss, Guillaume Evin, and Caroline Le Bouteiller
Nat. Hazards Earth Syst. Sci., 23, 1769–1787, https://doi.org/10.5194/nhess-23-1769-2023, https://doi.org/10.5194/nhess-23-1769-2023, 2023
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In mountain catchments, damage during floods is generally primarily driven by the supply of a massive amount of sediment. Predicting how much sediment can be delivered by frequent and infrequent events is thus important in hazard studies. This paper uses data gathered during the maintenance operation of about 100 debris retention basins to build simple equations aiming at predicting sediment supply from simple parameters describing the upstream catchment.
Elsa S. Culler, Ben Livneh, Balaji Rajagopalan, and Kristy F. Tiampo
Nat. Hazards Earth Syst. Sci., 23, 1631–1652, https://doi.org/10.5194/nhess-23-1631-2023, https://doi.org/10.5194/nhess-23-1631-2023, 2023
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Landslides have often been observed in the aftermath of wildfires. This study explores regional patterns in the rainfall that caused landslides both after fires and in unburned locations. In general, landslides that occur after fires are triggered by less rainfall, confirming that fire helps to set the stage for landslides. However, there are regional differences in the ways in which fire impacts landslides, such as the size and direction of shifts in the seasonality of landslides after fires.
Stefan Steger, Mateo Moreno, Alice Crespi, Peter James Zellner, Stefano Luigi Gariano, Maria Teresa Brunetti, Massimo Melillo, Silvia Peruccacci, Francesco Marra, Robin Kohrs, Jason Goetz, Volkmar Mair, and Massimiliano Pittore
Nat. Hazards Earth Syst. Sci., 23, 1483–1506, https://doi.org/10.5194/nhess-23-1483-2023, https://doi.org/10.5194/nhess-23-1483-2023, 2023
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We present a novel data-driven modelling approach to determine season-specific critical precipitation conditions for landslide occurrence. It is shown that the amount of precipitation required to trigger a landslide in South Tyrol varies from season to season. In summer, a higher amount of preparatory precipitation is required to trigger a landslide, probably due to denser vegetation and higher temperatures. We derive dynamic thresholds that directly relate to hit rates and false-alarm rates.
Yaspal Sundriyal, Vipin Kumar, Neha Chauhan, Sameeksha Kaushik, Rahul Ranjan, and Mohit Kumar Punia
Nat. Hazards Earth Syst. Sci., 23, 1425–1431, https://doi.org/10.5194/nhess-23-1425-2023, https://doi.org/10.5194/nhess-23-1425-2023, 2023
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The NW Himalaya has been one of the most affected terrains of the Himalaya, subject to disastrous landslides. This article focuses on two towns (Joshimath and Bhatwari) of the NW Himalaya, which have been witnessing subsidence for decades. We used a slope stability simulation to determine the response of the hillslopes accommodating these towns under various loading conditions. We found that the maximum displacement in these hillslopes might reach up to 20–25 m.
Yu Zhuang, Aiguo Xing, Perry Bartelt, Muhammad Bilal, and Zhaowei Ding
Nat. Hazards Earth Syst. Sci., 23, 1257–1266, https://doi.org/10.5194/nhess-23-1257-2023, https://doi.org/10.5194/nhess-23-1257-2023, 2023
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Tree destruction is often used to back calculate the air blast impact region and to estimate the air blast power. Here we established a novel model to assess air blast power using tree destruction information. We find that the dynamic magnification effect makes the trees easier to damage by a landslide-induced air blast, but the large tree deformation would weaken the effect. Bending and overturning are two likely failure modes, which depend heavily on the properties of trees.
Suzanne Lapillonne, Firmin Fontaine, Frédéric Liebault, Vincent Richefeu, and Guillaume Piton
Nat. Hazards Earth Syst. Sci., 23, 1241–1256, https://doi.org/10.5194/nhess-23-1241-2023, https://doi.org/10.5194/nhess-23-1241-2023, 2023
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Debris flows are fast flows most often found in torrential watersheds. They are composed of two phases: a liquid phase which can be mud-like and a granular phase, including large boulders, transported along with the flow. Due to their destructive nature, accessing features of the flow, such as velocity and flow height, is difficult. We present a protocol to analyse debris flow data and results of the Réal torrent in France. These results will help experts in designing models.
Carlos Millán-Arancibia and Waldo Lavado-Casimiro
Nat. Hazards Earth Syst. Sci., 23, 1191–1206, https://doi.org/10.5194/nhess-23-1191-2023, https://doi.org/10.5194/nhess-23-1191-2023, 2023
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This study is the first approximation of regional rainfall thresholds for shallow landslide occurrence in Peru. This research was generated from a gridded precipitation data and landslide inventory. The analysis showed that the threshold based on the combination of mean daily intensity–duration variables gives the best results for separating rainfall events that generate landslides. Through this work the potential of thresholds for landslide monitoring at the regional scale is demonstrated.
Luca Verrucci, Giovanni Forte, Melania De Falco, Paolo Tommasi, Giuseppe Lanzo, Kevin W. Franke, and Antonio Santo
Nat. Hazards Earth Syst. Sci., 23, 1177–1190, https://doi.org/10.5194/nhess-23-1177-2023, https://doi.org/10.5194/nhess-23-1177-2023, 2023
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Stability analyses in static and seismic conditions were performed on four rockslides that occurred during the main shocks of the 2016–2017 central Italy seismic sequence. These results also indicate that specific structural features of the slope must carefully be accounted for in evaluating potential hazards on transportation infrastructures in mountainous regions.
Enner Alcântara, José A. Marengo, José Mantovani, Luciana R. Londe, Rachel Lau Yu San, Edward Park, Yunung Nina Lin, Jingyu Wang, Tatiana Mendes, Ana Paula Cunha, Luana Pampuch, Marcelo Seluchi, Silvio Simões, Luz Adriana Cuartas, Demerval Goncalves, Klécia Massi, Regina Alvalá, Osvaldo Moraes, Carlos Souza Filho, Rodolfo Mendes, and Carlos Nobre
Nat. Hazards Earth Syst. Sci., 23, 1157–1175, https://doi.org/10.5194/nhess-23-1157-2023, https://doi.org/10.5194/nhess-23-1157-2023, 2023
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The municipality of Petrópolis (approximately 305 687 inhabitants) is nestled in the mountains 68 km outside the city of Rio de Janeiro. On 15 February 2022, the city of Petrópolis in Rio de Janeiro, Brazil, received an unusually high volume of rain within 3 h (258 mm). This resulted in flash floods and subsequent landslides that caused 231 fatalities, the deadliest landslide disaster recorded in Petrópolis. This work shows how the disaster was triggered.
Joshua N. Jones, Georgina L. Bennett, Claudia Abancó, Mark A. M. Matera, and Fibor J. Tan
Nat. Hazards Earth Syst. Sci., 23, 1095–1115, https://doi.org/10.5194/nhess-23-1095-2023, https://doi.org/10.5194/nhess-23-1095-2023, 2023
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We modelled where landslides occur in the Philippines using landslide data from three typhoon events in 2009, 2018, and 2019. These models show where landslides occurred within the landscape. By comparing the different models, we found that the 2019 landslides were occurring all across the landscape, whereas the 2009 and 2018 landslides were mostly occurring at specific slope angles and aspects. This shows that landslide susceptibility must be considered variable through space and time.
Shalev Siman-Tov and Francesco Marra
Nat. Hazards Earth Syst. Sci., 23, 1079–1093, https://doi.org/10.5194/nhess-23-1079-2023, https://doi.org/10.5194/nhess-23-1079-2023, 2023
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Debris flows represent a threat to infrastructure and the population. In arid areas, they are observed when heavy rainfall hits steep slopes with sediments. Here, we use digital surface models and radar rainfall data to detect and characterize the triggering and non-triggering rainfall conditions. We find that rainfall intensity alone is insufficient to explain the triggering. We suggest that antecedent rainfall could represent a critical factor for debris flow triggering in arid regions.
Xun Huang, Zhijian Zhang, and Guoping Xiang
Nat. Hazards Earth Syst. Sci., 23, 871–889, https://doi.org/10.5194/nhess-23-871-2023, https://doi.org/10.5194/nhess-23-871-2023, 2023
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A sensitivity analysis on the building impact force resulting from the representative built environment parameters is executed through the FLOW-3D model. The surrounding buildings' properties, especially the azimuthal angle, have been confirmed to play significant roles in determining the peak impact forces. The single and combined effects of built environments are analyzed in detail. This will improve understanding of vulnerability assessment and migration design against debris flow hazards.
Jean-Claude Maki Mateso, Charles L. Bielders, Elise Monsieurs, Arthur Depicker, Benoît Smets, Théophile Tambala, Luc Bagalwa Mateso, and Olivier Dewitte
Nat. Hazards Earth Syst. Sci., 23, 643–666, https://doi.org/10.5194/nhess-23-643-2023, https://doi.org/10.5194/nhess-23-643-2023, 2023
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This research highlights the importance of human activities on the occurrence of landslides and the need to consider this context when studying hillslope instability patterns in regions under anthropogenic pressure. Also, this study highlights the importance of considering the timing of landslides and hence the added value of using historical information for compiling an inventory.
Jakob Rom, Florian Haas, Tobias Heckmann, Moritz Altmann, Fabian Fleischer, Camillo Ressl, Sarah Betz-Nutz, and Michael Becht
Nat. Hazards Earth Syst. Sci., 23, 601–622, https://doi.org/10.5194/nhess-23-601-2023, https://doi.org/10.5194/nhess-23-601-2023, 2023
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In this study, an area-wide slope-type debris flow record has been established for Horlachtal, Austria, since 1947 based on historical and recent remote sensing data. Spatial and temporal analyses show variations in debris flow activity in space and time in a high-alpine region. The results can contribute to a better understanding of past slope-type debris flow dynamics in the context of extreme precipitation events and their possible future development.
Tom Birien and Francis Gauthier
Nat. Hazards Earth Syst. Sci., 23, 343–360, https://doi.org/10.5194/nhess-23-343-2023, https://doi.org/10.5194/nhess-23-343-2023, 2023
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On highly fractured rockwalls such as those found in northern Gaspésie, most rockfalls are triggered by weather conditions. This study highlights that in winter, rockfall frequency is 12 times higher during a superficial thaw than during a cold period in which temperature remains below 0 °C. In summer, rockfall frequency is 22 times higher during a heavy rainfall event than during a mainly dry period. This knowledge could be used to implement a risk management strategy.
Cited articles
Aaron, J. and Hungr, O.: Dynamic analysis of an extraordinarily mobile rock
avalanche in the Northwest Territories, Canada, Can. Geotech. J., 53,
899–908, https://doi.org/10.1139/cgj-2015-0371, 2016.
Aguilar, G., Carretier, S., Regard, V., Vassallo, R., Riquelme, R., and
Martinod, J.: Grain size-dependent 10Be concentrations in alluvial stream
sediment of the Huasco Valley, a semi-arid Andes region, Quaternary
Geochronol., 19, 163–172, https://doi.org/10.1016/j.quageo.2013.01.011,
2014.
Alganci, U., Besol, B., and Sertel, E.: Accuracy Assessment of Different
Digital Surface Models, ISPRS Int. J. Geo.-Inf., 7, 114, https://doi.org/10.3390/ijgi7030114,
2018.
Alimohammadlou, Y., Najafi, A., and Yalcin, A.: Landslide process and
impacts: A proposed classification method, CATENA, 104, 219–232,
https://doi.org/10.1016/j.catena.2012.11.013, 2013.
ASTM: D2216-19, Standard Test Methods for Laboratory Determination of Water
(Moisture) Content of Soil and Rock by Mass, ASTM International, West
Conshohocken, PA, 2019, https://doi.org/10.1520/D2216-19, 2019.
ASTM: D3080/D3080M-11: Standard Test Method for Direct Shear Test of Soils
Under Consolidated Drained Conditions (Withdrawn 2020), ASTM International,
West Conshohocken, PA, 2011, https://doi.org/10.1520/d3080_d3080m-11, 2020.
Bühler, Y., Christen, M., Kowalski, J., and Bartelt, P.: Sensitivity of
snow avalanche simulations to digital elevation model quality and
resolution, Ann. Glaciol., 52, 72–80,
https://doi.org/10.3189/172756411797252121, 2011.
Bueechi, E., Klimeš, J., Frey, H., Huggel, C., Strozzi, T., and
Cochachin, A.: Regional-scale landslide susceptibility modelling in the
Cordillera Blanca, Peru – a comparison of different approaches, Landslides,
16, 395–407, https://doi.org/10.1007/s10346-018-1090-1, 2018.
Calhoun, N. C. and Clague, J. J.: Distinguishing between debris flows and
hyperconcentrated flows: an example from the eastern Swiss Alps, Earth Surf.
Proc. Land., 43, 1280–1294,
https://doi.org/10.1002/esp.4313, 2018.
Cembrano, J. and Lara, L.: The link between volcanism and tectonics in the
southern volcanic zone of the Chilean Andes: A review, Tectonophysics, 471,
96–113, https://doi.org/10.1016/j.tecto.2009.02.038, 2009.
Dufresne, A., Wolken, G. J., Hibert, C., Bessette-Kirton, E. K., Coe, J. A.,
Geertsema, M., and Ekström, G.: The 2016 Lamplugh rock avalanche,
Alaska: deposit structures and emplacement dynamics, Landslides, 16,
2301–2319, https://doi.org/10.1007/s10346-019-01225-4, 2019.
Evans, S. G., Bishop, N. F., Fidel Smoll, L., Valderrama Murillo, P.,
Delaney, K. B., and Oliver-Smith, A.: A re-examination of the mechanism and
human impact of catastrophic mass flows originating on Nevado Huascarán,
Cordillera Blanca, Peru in 1962 and 1970, Eng. Geol., 108, 96–118,
https://doi.org/10.1016/j.enggeo.2009.06.020, 2009.
Fustos, I., Abarca-del-Rio, R., Moreno-Yaeger, P., and Somos-Valenzuela, M.:
Rainfall-Induced Landslides forecast using local precipitation and global
climate indexes, Nat. Hazards, 102, 115–131,
https://doi.org/10.1007/s11069-020-03913-0, 2020.
García-Delgado, H., Machuca, S., and Medina, E.: Dynamic and geomorphic
characterizations of the Mocoa debris flow (March 31, 2017, Putumayo
Department, southern Colombia), Landslides, 16, 597–609,
https://doi.org/10.1007/s10346-018-01121-3, 2019.
Garrido, N.: Deslizamientos y flujos de detritos en Petrohué, Sierra
Santo Domingo, naciente río Petrohué ladera sur. 02.06.2015.
Servicio Nacional de Geología y Minería, Informe Técnico, 11 pp., 2015.
Garrido, N., Mella, M., Sepúlveda, V., Duhart, P., and Moreno, H.: Efectos
geológicos de los flujos de detritos ruta CH-225 entre Ensenada y
Petrohué, 08 de enero 2017, región de Los Lagos (INF-X-05.2017)
[informe inédito], Puerto Varas: Sernageomin, 2017, 12, 2017.
Garrido, N., Sepúlveda, V., Duhart, P.: Catastro de remociones en masa
de la Provincia de Llanquihue, Región de Los Lagos (INF-Los
Lagos-10.2018) [informe inédito], Puerto Varas, Sernageomin, 2018.
INE: ENCUESTA MENSUAL DE ALOJAMIENTO TURÍSTICO, AÑO 2017, Technical
report, available at:
https://www.ine.cl/docs/default-source/actividad-del-turismo/publicaciones-y-anuarios/informe-anual/informe-anual-emat-2017.pdf
(last access: 12 June 2020), 2018.
Jakob, M., Hungr, O., and Jakob, D. M.: Debris-flow Hazards and Related
Phenomena, Springer, Berlin, Heidelberg, 2005.
Johnson, J. B. and Palma, J. L.: Lahar infrasound associated with Volcán
Villarrica's 3 March 2015 eruption, Geophys. Res. Lett., 42, 6324–6331,
https://doi.org/10.1002/2015gl065024, 2015.
Kääb, A., Huggel, C., Fischer, L., Guex, S., Paul, F., Roer, I., Salzmann, N., Schlaefli, S., Schmutz, K., Schneider, D., Strozzi, T., and Weidmann, Y.: Remote sensing of glacier- and permafrost-related hazards in high mountains: an overview, Nat. Hazards Earth Syst. Sci., 5, 527–554, https://doi.org/10.5194/nhess-5-527-2005, 2005.
Korup, O., Seidemann, J., and Mohr, C. H.: Increased landslide activity on
forested hillslopes following two recent volcanic eruptions in Chile, Nat.
Geosci., 12, 284–289, https://doi.org/10.1038/s41561-019-0315-9, 2019.
Lavigne, F. and Suwa, H.: Contrasts between debris flows, hyperconcentrated
flows and stream flows at a channel of Mount Semeru, East Java, Indonesia,
Geomorphology, 61, 41–58, https://doi.org/10.1016/j.geomorph.2003.11.005,
2004.
Major, J. J., Bertin, D., Pierson, T. C., Amigo, Á., Iroumé, A.,
Ulloa, H., and Castro, J.: Extraordinary sediment delivery and rapid
geomorphic response following the 2008–2009 eruption of Chaitén Volcano,
Chile, Water Resour. Res., 52, 5075–5094,
https://doi.org/10.1002/2015wr018250, 2016.
Martha, T. R., Kerle, N., Jetten, V., van Westen, C. J., and Kumar, K. V.:
Characterising spectral, spatial and morphometric properties of landslides
for semi-automatic detection using object-oriented methods, Geomorphology,
116, 24–36, https://doi.org/10.1016/j.geomorph.2009.10.004, 2010.
Mergili, M. and Pudasaini, S. P.:. r.avaflow – The mass flow simulation tool, available at: https://www.landslidemodels.org/r.avaflow/ (last access: 7 October 2021), 2014–2021.
Mergili, M., Fischer, J.-T., Krenn, J., and Pudasaini, S. P.: r.avaflow v1, an advanced open-source computational framework for the propagation and interaction of two-phase mass flows, Geosci. Model Dev., 10, 553–569, https://doi.org/10.5194/gmd-10-553-2017, 2017.
Mergili, M., Frank, B., Fischer, J.-T., Huggel, C., and Pudasaini, S. P.:
Computational experiments on the 1962 and 1970 landslide events at
Huascarán (Peru) with r.avaflow: Lessons learned for predictive mass
flow simulations, Geomorphology, 322, 15–28,
https://doi.org/10.1016/j.geomorph.2018.08.032, 2018a.
Mergili, M., Emmer, A., Juřicová, A., Cochachin, A., Fischer, J.-T.,
Huggel, C., and Pudasaini, S. P.: How well can we simulate complex
hydro-geomorphic process chains? The 2012 multi-lake outburst flood in the
Santa Cruz Valley (Cordillera Blanca, Perú), Earth Surf. Proc.
Land., 43, 1373–1389, https://doi.org/10.1002/esp.4318, 2018b.
Moreno, H., Varela, J., López-E,L., Munizaga, F., and Lahsen, A.:
Geología y riesgo volcánico del volcán Osorno y centros
eruptivos menores, Universidad de Chile, Departamento de Geología y
Geofisica, Sangiago, 212 pp., 1985.
Moreno, H., Lara, L. E., and Orozco, G.: Geología del volcán Osorno,
Región de Los Lagos, Servicio Nacional de Geología y Minería,
Carta Geológica de Chile, Serie Geología Básica 126: p., 1 mapa
escala 1:50.000, Santiago, 2010.
Moreno, T. and Gibbons, W. (Eds.): The Geology of Chile, The Geological Society of London, https://doi.org/10.1144/goch, 2007.
Naranjo, J. L., Sigurdsson, H., Carey, S. N., and Fritz, W.: Eruption of the
Nevado del Ruiz Volcano, Colombia, On 13 November 1985: Tephra Fall and
Lahars, Science, 233, 961–963,
https://doi.org/10.1126/science.233.4767.961, 1986.
Oyarzún, J.: Análisis de los factores gatillantes al flujo
hiperconcentrado en Villa Santa Lucía y determinación de las
condicionantes de un proceso futuro, Trabajo de Proyecto de Titulación
para optar al Título de Ingeniero Civil, Universidad de La Frontera,
Facultad de Ingeniería y Ciencias, 2019.
Pierson, T. C.: Flow characteristics of large eruption-triggered debris
flows at snow-clad volcanoes: constraints for debris-flow models, J.
Volcanol. Geoth. Res., 66, 283–294,
https://doi.org/10.1016/0377-0273(94)00070-w, 1995.
Pierson, T. C., Major, J. J., Amigo, Á., and Moreno, H.: Acute sedimentation response to rainfall following the explosive phase of the 2008–2009 eruption of Chaitén volcano, Chile, Bull. Volcanol., 75, 723, https://doi.org/10.1007/s00445-013-0723-4, 2013.
Pudasaini, S. P.: A general two-phase debris flow model, J. Geophys. Res.,
117, F03010, https://doi.org/10.1029/2011jf002186, 2012.
Pudasaini, S. P. and Mergili, M.: A Multi-Phase Mass Flow Model, J.
Geophys. Res.-Earth, 124, 2920–2942,
https://doi.org/10.1029/2019jf005204, 2019.
Qin, C.-Z., Bao, L.-L., Zhu, A.-X., Wang, R.-X., and Hu, X.-M.: Uncertainty
due to DEM error in landslide susceptibility mapping, Int. J.
Geogr. Inf. Sci., 27, 1364–1380,
https://doi.org/10.1080/13658816.2013.770515, 2013.
Rodríguez, I., Páez, J., van Wyk de Vries, M. S., van Wyk de Vries,
B., and Godoy, B.: Dynamics and physical parameters of the Lastarria debris
avalanche, Central Andes, J. Volcanol. Geoth. Res.,
402, 106990, https://doi.org/10.1016/j.jvolgeores.2020.106990, 2020.
Schaefer, L. N., Kennedy, B. M., Villeneuve, M. C., Cook, S. C. W., Jolly,
A. D., Keys, H. J. R., and Leonard, G. S.: Stability assessment of the
Crater Lake/Te Wai-ā-moe overflow channel at Mt. Ruapehu (New Zealand),
and implications for volcanic lake break-out triggers, J.
Volcanol. Geoth. Res., 358, 31–44,
https://doi.org/10.1016/j.jvolgeores.2018.06.011, 2018.
Schuster, R. L., NietoThomas, A. S., D. O'Rourke, T., Crespo, E., and
Plaza-Nieto, G.: Mass wasting triggered by the 5 March 1987 ecuador
earthquakes, Eng. Geol., 42, 1–23,
https://doi.org/10.1016/0013-7952(95)00024-0, 1996.
Sepúlveda, S. A., Moreiras, S. M., Lara, M., and Alfaro, A.: Debris
flows in the Andean ranges of central Chile and Argentina triggered by 2013
summer storms: characteristics and consequences, Landslides, 12, 115–133,
https://doi.org/10.1007/s10346-014-0539-0, 2014.
Sheridan, M. F., Stinton, A. J., Patra, A., Pitman, E. B., Bauer, A., and
Nichita, C. C.: Evaluating Titan2D mass-flow model using the 1963 Little
Tahoma Peak avalanches, Mount Rainier, Washington, J. Volcanol.
Geoth. Res., 139, 89–102,
https://doi.org/10.1016/j.jvolgeores.2004.06.011, 2005.
Shu, H., Ma, J., Yu, H., Hürlimann, M., Zhang, P., Liu, F., and Qi, S.:
Effect of Density and Total Weight on Flow Depth, Velocity, and Stresses in
Loess Debris Flows, Water, 10, 1784, https://doi.org/10.3390/w10121784,
2018.
Sosio, R., Crosta, G. B., and Hungr, O.: Numerical modeling of debris
avalanche propagation from collapse of volcanic edifices, Landslides, 9,
315–334, https://doi.org/10.1007/s10346-011-0302-8, 2011.
Somos-Valenzuela, M. A., Oyarzún-Ulloa, J. E., Fustos-Toribio, I. J., Garrido-Urzua, N., and Chen, N.: The mudflow disaster at Villa Santa Lucía in Chilean Patagonia: understandings and insights derived from numerical simulation and postevent field surveys, Nat. Hazards Earth Syst. Sci., 20, 2319–2333, https://doi.org/10.5194/nhess-20-2319-2020, 2020.
Stern, C. R.: Holocene tephrochronology record of large explosive eruptions
in the southernmost Patagonian Andes, B. Volcanol., 70, 435–454,
https://doi.org/10.1007/s00445-007-0148-z, 2007.
Tacconi Stefanelli, C., Vilímek, V., Emmer, A., and Catani, F.:
Morphological analysis and features of the landslide dams in the Cordillera
Blanca, Peru, Landslides, 15, 507–521,
https://doi.org/10.1007/s10346-017-0888-6, 2017.
Thouret, J.-C., Antoine, S., Magill, C., and Ollier, C.: Lahars and debris
flows: Characteristics and impacts, Earth-Sci. Rev., 201, 103003,
https://doi.org/10.1016/j.earscirev.2019.103003, 2020.
Vezzoli, L., Apuani, T., Corazzato, C., and Uttini, A.: Geological and
geotechnical characterization of the debris avalanche and pyroclastic
deposits of Cotopaxi Volcano (Ecuador). A contribute to instability-related
hazard studies, J. Volcanol. Geoth. Res., 332, 51–70,
https://doi.org/10.1016/j.jvolgeores.2017.01.004, 2017.
Wieczorek, G. F., Larsen, M. C., and Eaton, L. S.: Catastrophic landslides and
flooding in coastal Venezuela, December 16, 1999 (abstr.). In Program with
abstracts, 2000 Annual Meeting, Assoc. of Engrg. Geologists, San Jose,
California, 19–26 September, AEG News, Vol. 43, p. 120, 2000.
Zwinger, T., Kluwick, A., and Sampl, P.: Numerical Simulation of Dry-Snow
Avalanche Flow over Natural Terrain, in: Dynamic Response of Granular and
Porous Materials under Large and Catastrophic Deformations, Springer Berlin
Heidelberg, 161–194,
https://doi.org/10.1007/978-3-540-36565-5_5, 2003.
Short summary
Links between debris flow and volcanic evolution are an open question in the southern Andes. We modelled the catastrophic debris flow using field data, a geotechnical approach and numerical modelling of the Petrohué event (Chile, 2017). Our results indicated new debris-flow-prone zones. Finally, we propose considering connections between volcanoes and debris flow in the southern Andes.
Links between debris flow and volcanic evolution are an open question in the southern Andes. We...
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