Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
Reactive slabs of wind-drifted snow will form as new snow piles up and is easily blown by strong W/SW winds. These slabs will be most prevalent on the downwind sides of ridges, below cornices and cliffbands, and on mid-slope rollovers. These slabs may range from soft near treeline to stiffer and more consequential in alpine terrain.
Your best tool to manage your exposure to this problem will be visual clues. Look for blowing snow, sharp cornice formation, and dune-like drifts to help you identify where the wind has built slabs. As you move around, you can use small test slopes to help you gauge slab reactivity.
Steer around steep wind-loaded features, especially above 6000 ft, where slabs could pack a bigger punch. Shooting cracks or recent avalanches are great reasons to pump the brakes and stick to lower-angled terrain.
Additional Discussion:
Triggering avalanches in more sheltered terrain may become possible if you find over 6-8 inches of new snow. If this occurs, look for storm snow instabilities before engaging with steep slopes over 35 degrees.
(2/17/2025)
Pay attention to blowing snow and sharp drifts like this to help you pinpoint where slabs have formed.
Photo: Joe Dellaporta