Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2
You could trigger wind slabs up to 3 feet thick in exposed terrain. Days of loading wind speeds formed slabs, drifts, and cornices near upper elevation ridgelines and in some middle elevation terrain, and today's winds may continue building slabs and wind features. In the craggy Sawtooth Mtns, watch for stiff pillows of snow at the bottom of large cliff faces, chutes, and couloirs.
The fresh slabs rest above persistent weak layers (crusts, crusts + facets, facets, and possibly surface hoar) on many slopes. How could they behave?
- Natural cornice fall could trigger wind slabs
- You could trigger slabs remotely (from above, below, or to the side) - see photo
- They could be very sensitive to your weight, even where the slabs are quite soft
- Avalanches may be wider than you expect
Cornices, drifts, dunes, rippled snow surfaces, and chalky snow pillows are visible clues that the wind has been at work. Give large or overhanging cornices a wide berth. If you see cracks shooting out in front of your skis or boards, you've probably found a wind slab. If you feel the snow stiffen beneath your sled or skis, its time to steer clear of large or consequential avalanche paths.
(2/27/2024) This slab avalanche was triggered Tuesday from 50 ft away on a low-angle ridgeline. It broke widely in wind-drifted snow on a thin layer of facets above a crust. Cracks extended another 100' cross-slope beyond the crown. Smiley Ck, ENE @ 9,100'.
Photo: Sawtooth Avalanche Center