Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Strong winds will continue to deposit snow into leeward terrain features wherever there is still snow available for transport. Unstable wind slabs have and may continue to form on a variety of surface types, which will affect their size and sensitivity. Localized assessment of snow surfaces and what is just beneath the snow surface will be important to understand where this problem lies. Protected areas that have held soft snow, and areas with re-faceting surfaces are where this problem is most likely to be reactive. Look for blowing snow and cornice formation as signs of active loading. Hollow, stiff, textured snow in start zones, gullies, and bowls can alert you to the problem today. Keep in mind - a small wind slab avalanche in extreme terrain can have extreme consequences.
(3/9/2024) Photo: Eastern Sierra Avalanche Center