2015
DOI: 10.5194/nhess-15-757-2015
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Secondary lahar hazard assessment for Villa la Angostura, Argentina, using Two-Phase-Titan modelling code during 2011 Cordón Caulle eruption

Abstract: Abstract. This paper presents the results of lahar modelling in the town of Villa La Angostura (Neuquén-Argentina) based on the Two-Phase-Titan modelling computer code. The purpose of this exercise is to provide decision makers with a useful tool to assess lahar hazard during the 2011 PuyehueCordón Caulle Volcanic Complex eruption. The possible occurrence of lahars mobilized from recent ash falls that could reach the city was analysed. The performance of the TwoPhase-Titan model using 15 m resolution digital e… Show more

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Cited by 31 publications
(27 citation statements)
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“…The geomorphology of volcanoes has long been used to investigate volcanic development and activity (Thouret, 1999). Digital topography has been used to classify volcano morphology (e.g., Euillades et al, 2013;Favalli et al, 1999;Grosse et al, 2014;Pedersen & Grosse, 2014;Prima & Yoshida, 2010), identify and assess eruptive deposits and structures (e.g., Csatho et al, 2008;Hofton et al, 2006;Hutchison et al, 2015;Zouzias et al, 2011), and evaluate ongoing volcanic hazards (e.g., Favalli et al, 2005;Córdoba et al, 2015;Stefanescu et al, 2012). Many studies have used the morphometry of lava flow deposits (e.g., Nomikou et al, 2014;Pyle & Elliott, 2006;Tarquini et al, 2012;Ventura & Vilardo, 2007), cones (e.g., Fornaciai et al, 2012;Kervyn et al, 2012), and other deposits (e.g., Jessop et al, 2012) to investigate their rheology and dynamics of emplacement.…”
Section: Introductionmentioning
confidence: 99%
“…The geomorphology of volcanoes has long been used to investigate volcanic development and activity (Thouret, 1999). Digital topography has been used to classify volcano morphology (e.g., Euillades et al, 2013;Favalli et al, 1999;Grosse et al, 2014;Pedersen & Grosse, 2014;Prima & Yoshida, 2010), identify and assess eruptive deposits and structures (e.g., Csatho et al, 2008;Hofton et al, 2006;Hutchison et al, 2015;Zouzias et al, 2011), and evaluate ongoing volcanic hazards (e.g., Favalli et al, 2005;Córdoba et al, 2015;Stefanescu et al, 2012). Many studies have used the morphometry of lava flow deposits (e.g., Nomikou et al, 2014;Pyle & Elliott, 2006;Tarquini et al, 2012;Ventura & Vilardo, 2007), cones (e.g., Fornaciai et al, 2012;Kervyn et al, 2012), and other deposits (e.g., Jessop et al, 2012) to investigate their rheology and dynamics of emplacement.…”
Section: Introductionmentioning
confidence: 99%
“…LLUNPIY, SCIDDICA-SS3, and SCIDDICA-SS2 are our most advanced models (in the sense that they include the features of the previous models plus other new ones) for simulating flow-like landslides and lahars. Unlike other models, which were used in lahar simulations (LAHARZ -e.g., Schilling, 1998;Muñoz-Salinas et al, 2009;TITAN2De.g., Sheridan et al, 2005;Williams et al, 2008;Córdoba et al, 2015), they allow the implementation of the erosion process.…”
Section: Multicomponent or Macroscopic Cellular Automatamentioning
confidence: 99%
“…Titan2F was developed to account for both of the phases keeping a reasonable computational cost [8], [21]. The fluid part of the flow is modeled using typical shallow water like approach, whereas the frictional behavior of the solid phase is accounted by assuming that Mohr-Coulomb law is valid in such case, as in [17] and [18].…”
Section: Modeling Lahars With Titan2fmentioning
confidence: 99%
“…The modeling techniques range from empirical or semi-empirical models (see for example [3], [4]) to models that consider the mechanics of their behavior (e.g. [5], [6], [7], [8]). Each kind of model have its own strengths and weakness.…”
Section: Introductionmentioning
confidence: 99%
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