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Regional Debris-Flow Hazard Assessments
Regional debris-flow hazard assessments provide consistent information on potential hazards over large areas, often with limited available data....
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Dating of multiple debris flow stages in the Sandaoqiao gully, Kangding, Eastern Tibetan Plateau: implications for regional tectonic and climate changes
Chronology of debris flow deposits (DFD) is crucially important in understanding fan evolution and assessing the risks of future extreme disaster...
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Regional Debris Flow Hazard Assessment of the Grdelica Gorge (Serbia)
Road infrastructure development is currently very intensive in Serbia. One such example is the Grdelica Gorge, where a new highway was aligned and...
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Debris-Flow Risk Assessment
Risk assessments can inform a wide variety of decisions related to debris flows, such as: Is the community safe enough? Where is mitigation needed?...
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Modelling of debris-flow susceptibility and propagation: a case study from Northwest Himalaya
The geological and geographical position of the Northwest Himalayas makes it a vulnerable area for mass movements particularly landslides and debris...
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Debris Flow Dating and Magnitude Reconstruction
Debris flows typically occur in mountain regions with high energy relief, complex geology and extreme climate conditions, where they often affect...
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Establishing a GIS-based evaluation method considering spatial heterogeneity for debris flow susceptibility map** at the regional scale
Susceptibility map** is an effective means of preventing debris flow disasters. However, previous studies have failed to solve spatial...
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A precipitation downscaling framework for regional warning of debris flows in mountainous areas
A timely warning system for debris-flow mitigation in mountainous areas is vital to decrease casualties. However, the lack of rainfall monitoring...
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Estimating the daily rainfall thresholds of regional debris flows in the Bailong River Basin, China
Debris flows pose a major threat to life and property in mountainous regions. Rainfall thresholds are an important component for providing an early...
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Post-wildfire debris-flow runout map** using geospatial analysis
Post-wildfire debris flows are a significant natural hazard that is becoming more prevalent because of climate change and increasing populations in...
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Land Use Planning on Debris-Flow Fans
Land use planning is the most influential option for managing levels of natural hazard risk, as high-risk land uses can be avoided before an event...
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Quantifying the impact of earthquakes and geological factors on spatial heterogeneity of debris-flow prone areas: A case study in the Hengduan Mountains
Understanding the spatial heterogeneity of debris-flow-prone areas holds significant implications for regional risk management, particularly in...
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Debris-Flow Watersheds and Fans: Morphology, Sedimentology and Dynamics
Debris flows typically originate in mountainous watersheds. At the base of these watersheds and where not truncated by a higher order stream or...
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Modeling of breaching parameters for debris flow dams
The debris flow dam is a common type of barrier dams, which shows significant differences from other types of barrier dam such as landslide dam,...
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Debris Flow Susceptibility Evaluation in Meizoseismal Region: A Case Study in Jiuzhaigou, China
Jiuzhaigou is situated on a mountain-canyon region and is famous for frequent tectonic activities. An abundance of loose co-seismic landslides and...
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Debris flow susceptibility and hazard assessment in Fushun based on hydrological response units
Fushun, located in Northeast China, is prone to debris flow disasters due to its complex topographical and geological conditions. In 2013,...
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Statistical Techniques for Debris-Flow Frequency–Magnitude Analyses
Debris flows are a curse where they interfere with the built environment because of their poor predictability, their long runout and high impact...
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Identifying potential debris flow hazards after the 2022 Mw 6.8 Luding earthquake in southwestern China
Earthquakes can generate large amounts of co-seismic landslide debris and unstable hillslopes, which supply abundant material sources for subsequent...
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Dynamic susceptibility assessment of debris flow hazard after a strong earthquake, Wenchuan County, Sichuan, China
Large amounts of co-seismic landslides provide abundant debris sources following a strong earthquake and are prone to initiate and generate debris...
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Influence of runoff on debris flow propagation at a catchment scale: a case study
Debris flow mobility can vary during propagation due to changes in flow volume and bulk flow behavior resulting from the absorption of water from...
