Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Wind slabs are becoming more stubborn to trigger with time. However, in some areas, these stiff wind slabs formed over weak snow layers that take longer to strengthen, and you could still trigger a large, hard slab avalanche. A few inches of fresh snow and another day of easterly winds also means you could find shallow new drifts to trigger a small avalanche. Winds have blown in multiple directions over the last few days, so look for wind slabs on various aspects or even mid-slope. Strong winds have pressed these slabs into firmer 1F-P hard slabs in exposed alpine terrain. Consider the high consequences of triggering a wind slab that breaks wider and deeper than expected if it fails on weak snow above the Early February Crust.
Use visual clues such as blowing snow and textured surfaces to help you identify where the wind has been at work. Be suspect of terrain features that encourage drifting, such as the leeward sides of ridgelines, alpine couloirs, gully features, and cross-loaded depressions. Dial it back if you notice shooting cracks, whumphs, or hollow-sounding snow.
(2/18/2024)
Triggering a wind slab in the wrong spot could result in a much larger and wider avalanche if it breaks on old snow above the Early February Crust.
Forecasters observed this 1-2 day-old avalanche in the Teanaway drainage on Sunday.
W aspect, 6200 ft
Photo: Katie Warren