Ts. Chalmers et B. Jamieson, Extrapolating the skier stability of buried surface hoar layers from studyplot measurements, COLD REG SC, 33(2-3), 2001, pp. 163-177
Buried layers of surface hoar pose a challenge to avalanche forecasters in
many areas, partly because some layers stabilise quickly and others remain
unstable for a month or more. This paper relates the measurements of two su
rface hoar layers in a study plot, one buried 30 December 1999 and the othe
r buried 21 February 2000, to skier-triggered slab avalanches within 100 ki
n of the study plot in the Columbia Mountains of western Canada.
The two surface hoar layers were monitored at a tree-line study slope at Ro
gers Pass every 4 to 8 days until the end of March 2000. Physical propertie
s of the slab (load, thickness, hardness profile), and weak layer (shear st
rength, temperature, temperature gradient, crystal size, crystal form) were
observed. Approximately once every 2 weeks, the weak layers were photograp
hed in the pit wall to document their texture. On the same days, disaggrega
ted crystals from the weak layers were photographed on a crystal screen.
The February 21 layer, which initially consisted of 4-6-mm crystals, was lo
aded more slowly by snowfall, gained strength and stability more slowly, yi
elded initially lower stability indices and released many more skier-trigge
red avalanches than the December 30 layer, which initially consisted of lar
ger, 10-20-mm crystals. Critical study plot values of load, shear strength,
and stability are compared with critical values measured adjacent to over
50 skier-triggered slab avalanches. The shear strength of the weak layer, c
alculated skier stability index Sk(38), layer thickness, and load on the we
ak layer show potential predictive value for the stabilisation of buried su
rface hoar layers. While the time series of photographs of separated crysta
ls shows distinct changes, the time series of photographs of the buried sur
face hoar layers in situ reveals little useful information on textural chan
ges other than thinning of the layers. (C) 2001 Elsevier Science B.V. All r
ights reserved.