Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Strong north winds will redistribute recent snow into thicker, stiffer slabs on lee slopes and in cross-loaded features (gullies, rollovers, below ridge crests). Wind slabs will be sensitive to human triggers, and rapid loading could produce natural avalanches.
The key concern today is not just the wind slab itself—it’s the potential for a wind-slab trigger to step down and release the deeper persistent weak layer. In that scenario, a small-to-moderate wind slab could initiate a much larger avalanche failing 2–3+ feet deep, with long propagation.
Avoid travel in wind-loaded terrain, and give start zones and runouts a wide berth.