Annals of Glaciology · 1989 · 18 citations · 7 references
Natural ResourcesEarth SciencesHydrologyFluid DynamicsHydrologic ModelingSnow HydrologyAvalanche HydrologyAvalanche ProcessesAvalanche ScienceSnow PhysicsSnowmelt ModelingSnowpack DynamicsAvalanche SimulationFinite Difference SchemesFluid Constitutive EquationsSnow Avalanche DynamicsSnowpack ModelingSteady FlowSteady Shear FlowTwo-dimensional Flow Modeling
The authors of this paper have previously, in 1987, outlined the development of a set of constitutive equations representing the behaviour of avalanching snow, and the resulting equations for fully developed steady shear flow. The present paper considers the development of non-steady two-dimensional shear flow together with the use of a finite-difference programme to calculate snow-avalanche velocities and flow heights in the run-out zone. The numerical results thus obtained are compared with full-scale experimental data. These comparisons indicate that front velocity and run-out distance are simulated well by the model, and that the predicted snow deposits are fairly well in agreement with those actually observed.
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A Two–Parameter Model of Snow–Avalanche Motion
R. Perla, Te‐Shiang Cheng, D. M. McClung · Journal of Glaciology · 1980 · 247 citations
Computer Modeling of Large Rock Slides
F. J. Trunk, J. D. Dent, T. E. Lang · Journal of Geotechnical Engineering · 1986 · 37 citations