Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2–3
Gale-force winds and feet of new snow will build large slabs of wind-drifted snow and fragile cornices on the downwind sides of ridges, open slopes, and exposed gullies. The largest and most unstable wind slabs will form on NW-N-NE-E-SE aspects in near and above treeline terrain. Large wind slab avalanches that fail under the weight of the new snow or a cornice failure (natural triggers) will likely occur. People could also trigger wind slab avalanches easily if they venture onto/near a wind-loaded slope. These could also cause the Dec 1 persistent weak layer to fail as they move downhill. This would result in much larger and deeper avalanches that could travel into below-treeline terrain and could break across terrain features.
Blowing snow and poor visibility today make accidentally stumbling onto a dangerous wind-loaded slope or close to the edge of a cornice easier. Today is a day to avoid all avalanche terrain.