Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–1.5
Increasing northeast winds throughout the day will drift recent snow and may form thin slabs on atypical aspects. Expect to find these features downwind of ridgelines, saddles, or on the sidewalls of cross-loaded gullies. As you gain elevation, slabs may increase in thickness and become more widespread. These may form on crusts, which makes them easier to trigger.
Fresh cornices, dunes, rippled snow surfaces, and areas with stiffer snow are telltale signs of wind transport. Cracking beneath your boards or machine is a sign of an unstable slab.
(3/9/2024)
Wind drifting that causes sculpted snow dunes, as shown in this photo, are identifying signs of wind transport.
Photo: Flathead Avalanche Center