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Natural Hazards and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 10 | Copyright
Nat. Hazards Earth Syst. Sci., 12, 3075-3090, 2012
https://doi.org/10.5194/nhess-12-3075-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Oct 2012

Research article | 18 Oct 2012

Parameterization of a numerical 2-D debris flow model with entrainment: a case study of the Faucon catchment, Southern French Alps

H. Y. Hussin1, B. Quan Luna2, C. J. van Westen3, M. Christen4, J.-P. Malet5, and Th. W. J. van Asch6 H. Y. Hussin et al.
  • 1CNR-IRPI, via Madonna Alta 126, 06128 Perugia, Italy
  • 2NGI, Norwegian Geotechnical Institute – ICG, International Centre for Geohazards, Sognsveien 72, 0855, Oslo, Norway
  • 3Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, P.O. Box 6, 7500 AA Enschede, The Netherlands
  • 4WSL, Swiss Federal Institute for Snow and Avalanche Research SLF, Flüelastrasse 11, 7260 Davos Dorf, Switzerland
  • 5Institut de Physique du Globe de Strasbourg, CNRS UMR 7516, Université de Strasbourg / EOST, 5 rue René Descartes, 67084 Strasbourg Cedex, France
  • 6Faculty of Geosciences, Utrecht University, Utrecht, The Netherlands

Abstract. The occurrence of debris flows has been recorded for more than a century in the European Alps, accounting for the risk to settlements and other human infrastructure that have led to death, building damage and traffic disruptions. One of the difficulties in the quantitative hazard assessment of debris flows is estimating the run-out behavior, which includes the run-out distance and the related hazard intensities like the height and velocity of a debris flow. In addition, as observed in the French Alps, the process of entrainment of material during the run-out can be 10–50 times in volume with respect to the initially mobilized mass triggered at the source area. The entrainment process is evidently an important factor that can further determine the magnitude and intensity of debris flows. Research on numerical modeling of debris flow entrainment is still ongoing and involves some difficulties. This is partly due to our lack of knowledge of the actual process of the uptake and incorporation of material and due the effect of entrainment on the final behavior of a debris flow. Therefore, it is important to model the effects of this key erosional process on the formation of run-outs and related intensities. In this study we analyzed a debris flow with high entrainment rates that occurred in 2003 at the Faucon catchment in the Barcelonnette Basin (Southern French Alps). The historic event was back-analyzed using the Voellmy rheology and an entrainment model imbedded in the RAMMS 2-D numerical modeling software. A sensitivity analysis of the rheological and entrainment parameters was carried out and the effects of modeling with entrainment on the debris flow run-out, height and velocity were assessed.

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