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Civil Engineering Information Management

Location:
United States
Posted:
November 18, 2012

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Resume:

Geophysical Research Abstracts

Vol. **, EGU****-*699-1, 2010

EGU General Assembly 2010

Author(s) 2010

Uncertainty Quanti cation on the Determination of Debris Flow Run-Out

for Quantitative Risk Analysis

Byron Quan Luna (1), Zenon Medina-Cetina (2), Jean-Philippe Mallet (3), Cees van Westen (1), and Victor Jetten

(1)

(1) United Nations University-ITC School for Disaster Geo-information Management, Enschede, The Netherlands

(********@***.**), (2) Zachry Department of Civil Engineering, Texas A&M University, College Station TX, USA

(*****@****.***), (3) CNRS - University of Strasbourg, School and Observatory of Earth Sciences, Strasbourg, France

In recent times, a number of dynamic run-out models for debris ows have been developed for risk analysis, for

the creation of zonation plans, and for the design of potential mitigation measures. Dynamic run-out models are

capable of characterizing the material distribution, the ow intensity, and the zone of potential impact. Estimating

the intensity of rapid landslides like debris ows is fundamental for quantifying the hazard on a speci c location.

Dynamic models allow the effect of released volumes as well as rheological behaviours to be modeled for

different scenarios. However, these models are still based on simple assumptions on the physical mechanisms

controlling the ow and are based on resistance parameters that cannot be measured directly during an event. As

a consequence, these models are associated with large uncertainties, which must be addressed in a proper risk

analysis.

This work introduces a systematic identi cation, characterization and propagation of the uncertainties present

in debris ow hazards analysis, with the aim of populating a joint probability density function of the input

parameters of a given debris ow model, when conditioned on eld observations. From this distribution, likely

model responses would allow for generating best estimates and con dence measures of extreme run-out distances.

To demonstrate the implementation of this method, a two-dimensional dynamic run-out model is considered that

solves the conservation equations of mass and momentum. This general methodology facilitates the consistent

combination of physical models with the available observations. Expected outputs like extension, depth and

velocity can be used as input into vulnerability and quantitative risk analysis for risk mapping and regulatory

zoning. The outlined procedure provides a useful way to produce hazard or risk maps for the typical case

where historical records are either poorly documented or even completely lacking, as well as characterizing the

con dence limits on the zoning of interest.



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