Probabilistic Identification of Debris‐Flow Pathways in Mountain Fans Within a Stochastic Framework

Abstract Debris flows are solid‐liquid mixtures originating in the upper part of mountain basins and routing downstream along incised channels. When the channel incises an open fan, the debris flow leaves the active channel and propagates downstream along a new pathway. This phenomenon is called an avulsion. We retrieve the most probable avulsion pathways leveraging a Monte Carlo approach based on using Digital Elevation Models (DEMs). Starting from LiDAR‐based DEMs, we build an ensemble of synthetic DEMs using a local Gaussian probability density function of local elevation values and obtain an ensemble of drainage networks using a gravity‐driven routing algorithm. The ensemble of drainage networks was used to obtain the most probable pathways of avulsions. We applied our methodology to a real monitored fan in the Dolomites (Northeastern Italian Alps) subjected to debris‐flow activity with avulsions. Our approach allows us to verify the consistency between the occurrence probability of a synthetic pathway and those that historically occurred. Furthermore, our approach can be used to predict future debris‐flow avulsions, assuming relevance in debris‐flow risk assessment and planning of debris‐flow control works.

Authors

Institutions

Publication Details

Journal
Journal of Geophysical Research Earth Surface
Published
2024-12-01
DOI
https://doi.org/10.1029/2024jf007946
Citations
12
Primary Topic
Landslides and related hazards
Type
article
Field-Weighted Citation Impact
8.52
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Probabilistic Identification of Debris‐Flow Pathways in Mountain Fans Within a Stochastic Framework

Carlo Gregoretti, Mauro Boreggio, Martino Bernard, Matteo Barbini et al.
12 citations
Journal of Geophysical Research Earth Surface
Landslides and related hazards
8.52
article

Probabilistic Identification of Debris‐Flow Pathways in Mountain Fans Within a Stochastic Framework

Carlo Gregoretti, Mauro Boreggio, Martino Bernard, Matteo Barbini, Massimiliano Schiavo
article en
12 citations

Abstract

Abstract Debris flows are solid‐liquid mixtures originating in the upper part of mountain basins and routing downstream along incised channels. When the channel incises an open fan, the debris flow leaves the active channel and propagates downstream along a new pathway. This phenomenon is called an avulsion. We retrieve the most probable avulsion pathways leveraging a Monte Carlo approach based on using Digital Elevation Models (DEMs). Starting from LiDAR‐based DEMs, we build an ensemble of synthetic DEMs using a local Gaussian probability density function of local elevation values and obtain an ensemble of drainage networks using a gravity‐driven routing algorithm. The ensemble of drainage networks was used to obtain the most probable pathways of avulsions. We applied our methodology to a real monitored fan in the Dolomites (Northeastern Italian Alps) subjected to debris‐flow activity with avulsions. Our approach allows us to verify the consistency between the occurrence probability of a synthetic pathway and those that historically occurred. Furthermore, our approach can be used to predict future debris‐flow avulsions, assuming relevance in debris‐flow risk assessment and planning of debris‐flow control works.

Journal of Geophysical Research Earth SurfaceVol. 129(12)
University of Padua (IT), University of Florida (US)
Sustainable cities and communities
Openalex Percentile: Top 3%
Landslides and related hazards
8.52
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.