Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
Recent human triggered avalanches and wind loading show instability persists near and above treeline. Wind slab avalanches in near treeline terrain the past few days were not large, but all occurred in relatively small terrain features that limited avalanche size. Expect larger avalanches above treeline. You are most likely to trigger a wind slab on steep, unsupported features like convex rolls, hanging slopes, and steeper areas around cliffs and cornices.
As you gain elevation or move into open terrain take note of changes in the snow surface. Is one side of a ridge wind scoured while the other is not? Does the snow change consistency from light and fluffy to denser and more supportable? Using a probe or ski pole to locate deeper drifts, digging hand pits, and testing on very small slopes are simple methods that let you evaluate the wind slab problem as you travel.
(12/13/2021)
Cross loaded terrain features on Shuksan Arm
Photo: Lee Lazzara