Topographic curvature effects in applied avalanche modeling

被引:89
作者
Fischer, Jan-Thomas [1 ]
Kowalski, Julia [2 ]
Pudasaini, Shiva P. [3 ]
机构
[1] BFW, Fed Res & Training Ctr Forests Nat Hazards & Land, Dept Nat Hazards & Alpine Timberline, A-6020 Innsbruck, Austria
[2] WSL Inst Snow & Avalanche Res SLF, CH-7260 Davos, Switzerland
[3] Univ Bonn, Dept Geodynam & Geophys, Steinmann Inst, D-53115 Bonn, Germany
关键词
Snow; Avalanche; Dynamics; Modeling; Natural terrain; Curvature; Centrifugal force; Friction coefficients; DRY GRANULAR MASSES; RAPID SHEAR FLOWS; FREE-SURFACE FLOW; OBLIQUE SHOCKS; SIMULATION; MOTION; RUNOUT;
D O I
10.1016/j.coldregions.2012.01.005
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper describes the implementation of topographic curvature effects within the RApid Mass MovementS (RAMMS) snow avalanche simulation toolbox. RAMMS is based on a model similar to shallow water equations with a Coulomb friction relation and the velocity dependent Voellmy drag. It is used for snow avalanche risk assessment in Switzerland. The snow avalanche simulation relies on back calculation of observed avalanches. The calibration of the friction parameters depends on characteristics of the avalanche track. The topographic curvature terms are not yet included in the above mentioned classical model. Here, we fundamentally improve this model by mathematically and physically including the topographic curvature effects. By decomposing the velocity dependent friction into a topography dependent term that accounts for a curvature enhancement in the Coulomb friction, and a topography independent contribution similar to the classical Voellmy drag, we construct a general curvature dependent frictional resistance, and thus propose new extended model equations. With three site-specific examples, we compare the apparent frictional resistance of the new approach, which includes topographic curvature effects, to the classical one. Our simulation results demonstrate substantial effects of the curvature on the flow dynamics e.g., the dynamic pressure distribution along the slope. The comparison of resistance coefficients between the two models demonstrates that the physically based extension presents an improvement to the classical approach. Furthermore a practical example highlights its influence on the pressure outline in the run out zone of the avalanche. Snow avalanche dynamics modeling natural terrain curvature centrifugal force friction coefficients. (C) 2012 Elsevier BA,. All rights reserved.
引用
收藏
页码:21 / 30
页数:10
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