Snow cover properties for skier triggering of avalanches

被引:68
作者
Schweizer, J
Jamieson, JB
机构
[1] Swiss Fed Inst Forest Snow & Avalanche Res, CH-7260 Davos, Switzerland
[2] Univ Calgary, Dept Geol & Geophys, Dept Civil Engn, Calgary, AB T2N 1N4, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
avalanche forecasting; avalanche formation; avalanche mechanics; skier triggering; snow cover stability; snow physical properties;
D O I
10.1016/S0165-232X(01)00039-8
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Snowpack characteristics for skier-triggered avalanches are described in order to better understand skier triggering, to improve snow profile observation and interpretation, to make suggestions for route selection and to provide a basis for further research. Our analysis is based on avalanche and snow profile data from skier-triggered avalanche sites in the Columbia Mountains of Canada and the Swiss Alps. Although these two mountain ranges have different climates, the characteristics for skier triggering are very similar. Whereas the snow cover in the profiles from the Columbia Mountains is more than twice as deep than in the ones from the Swiss Alps, the typical fracture depth (or slab thickness) is about the same (45 cm). Failure layer properties are very similar indicating favourable conditions for skier triggering and slab release. In both ranges, the failure layers are predominantly persistent, that is, they consist of crystals of surface hoar, facets and depth hoar, which are slow to metamorphose. The analysis has focussed on slab properties and weak layer properties, and in particular, their interaction. The findings support the simple model of skier loading in which skiers directly initiate failures in buried weak layers or interfaces. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:207 / 221
页数:15
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