Item: Case Study of a Deep Slab Instability and Associated Dry Avalanches
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Title: Case Study of a Deep Slab Instability and Associated Dry Avalanches
Proceedings: Proceedings of the 2000 International Snow Science Workshop, October 1-6, Big Sky, Montana
Authors:
- Bruce Jamieson [ Dept. of Civil Engineering, University of Calgary, Calgary, Alberta, T2N 1 N4, Canada ] [ Dept. of Geology and Geophysics, University of Calgary ]
- Torsten Geldsetzer [ Dept. of Civil Engineering, University of Calgary, Calgary, Alberta, T2N 1 N4, Canada ]
- Chris Stethem [ Chris Stethem and Associates, Canmore, Alberta, T1 W 2R8, Canada ]
Date: 2000
Abstract: This study considers the predictive merit of weather and snowpack data for avalanches that released throughout the winter on a layer of faceted crystals that formed on a rain crust in November 1996 in the North Columbia Mountains of western Canada. The facet-crust combinations formed as a result of a cold air mass cooling a layer of dry snow on top of a rain-wened layer. The highly ranked variables associated with natural avalanches include previous avalanche activity, accumulated snowfall over several days, changes in air temperature over four to five days, snowpack properties, including a shear frame stability index, and the difference in hardness between the facet layer and the crust. Increases in air temperature over four to five days correlate with increased avalanche activity, however current theories for warming do not explain decreased stability especially where the slab is thick. We argue that the fractures that release deep slab avalanches may be initiated where the slab is locally thin.
Language of Article: English
Presenters: Unknown
Keywords: avalanche forecasting, avalanche formation, faceted crystals, snow cover stability, snow cover structure, snow stratigraphy
Page Number(s): 101-108
Subjects: deep slab instability dry avalanches avalanche forecasting
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Digital Abstract Not Available
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