2004
DOI: 10.3189/172756404781814780
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Avalanche simulation with SAMOS

Abstract: Dry snow avalanches consist of two distinct layers. A dense-flow layer is superposed by a powder-snow layer, a cloud of relatively small ice particles suspended in air. The density of this suspension is one order of magnitude smaller than that of the dense flow. A simulation model for dry avalanches has been developed, based on separate sub-models for the two layers. The sub-models are coupled by an additional transition model, describing the exchange of mass and momentum between the layers. The fundamentals o… Show more

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Cited by 113 publications
(104 citation statements)
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“…Both models are in operational use by the Federal Service for Torrent, Erosion and Avalanche Control. A detailed description for the model SAMOS is given by Sailer et al (2002) and Sampl and Zwinger (2004). ELBA+ is an improved version of the model ELBA, which is described in-depth by Volk and Kleemayr (1999).…”
Section: Avalanche Processes and Modellingmentioning
confidence: 99%
“…Both models are in operational use by the Federal Service for Torrent, Erosion and Avalanche Control. A detailed description for the model SAMOS is given by Sailer et al (2002) and Sampl and Zwinger (2004). ELBA+ is an improved version of the model ELBA, which is described in-depth by Volk and Kleemayr (1999).…”
Section: Avalanche Processes and Modellingmentioning
confidence: 99%
“…To perform dynamic avalanche simulations with state-of-the-art software such as RAMMS (Christen et al, 2010) or SAMOS 25 (Sampl and Zwinger, 2004) an accurate identification of the release areas and the release volumes is mandatory. Prerequisites for triggering a snow slab avalanche can be summarized in three categories: (1) terrain, (2) snow cover specific and (3) meteorological factors (Schweizer et al, 2003).…”
Section: Introductionmentioning
confidence: 99%
“…In current engineering practice for hazard mapping and planning of long-term mitigation measures, release area size is a key input in numerical models of avalanche dynamics such as RAMMS (Christen et al, 2010) or SAMOS-AT (Sampl and Granig, 2009;Sampl and Zwinger, 2004). They allow the assessment of run-out, velocity, flow height or impact pressure of avalanches, and are especially important when historical data are sparse or completely lacking.…”
Section: Introductionmentioning
confidence: 99%