MoT-PSA: a two-layer depth-averaged model for simulation of powder snow avalanches on 3-D terrain

被引:2
|
作者
Vicari, Herve [1 ,2 ,3 ]
Issler, Dieter [1 ]
机构
[1] Norwegian Geotech Inst, Nat Hazards Div, POB 3930 Ulleval Stad, N-0806 Oslo, Norway
[2] WSL Inst Snow & Avalanche Res SLF, CH-7260 Davos, Switzerland
[3] Climate Change Extremes & Nat Hazards Alpine Reg R, CH-7260 Davos, Switzerland
关键词
deposition; depth-averaged numerical modelling; entrainment; hazard mapping; impact pressure; mixed snow avalanche; suspension layer; two layers; MASS-CHANGE MODEL; SCALING BEHAVIOR; FLOW; DYNAMICS;
D O I
10.1017/aog.2024.10
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
For snow-avalanche hazard mapping, one needs efficient tools that nevertheless capture the essential physical processes. The code MoT-PSA (Method of Transport - Powder Snow Avalanche) described here is based on the two-layer depth-averaged formulation for mixed snow avalanches developed by Eglit and co-workers in the 1980s but is extended to 3-D terrain and uses a fast numerical scheme based on the method of transport. Compared to previous works, we introduce novel formulations for the suspension and deposition of snow from the dense core. Snow cover and air entrainment are quantified with physics-based models. A sensitivity study of the model parameters on an idealized topography shows that both the dense core and the parameters of the powder snow cloud (PSC) governing particle suspension and settling significantly affect the dynamics. As expected, we observe that snow cover entrainment favours the formation of large PSCs with long runout. The powder-snow avalanche that occurred in Lom (Norway) on 27 February 2020 is back-calculated using MoT-PSA. With plausible parameter values, the model reproduces the dense core stopping at the gully's base and the dilute PSC travelling across the frozen lake for almost 1 km.
引用
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页数:16
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