Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
If you’re going to trigger a slab avalanche on Saturday, it will likely be in wind-effected terrain. With plenty of low-density snow available for transport, new shallow slabs may be forming throughout the day or you could still encounter lingering slabs from earlier on in the storm. Increasing winds on Saturday should have an easterly component to them, meaning you could see some atypical loading patterns including slabs forming on different aspects or slopes being more cross-loaded than you are used to. Use visual clues such as blowing snow, textured surfaces, new cornices, or drifts behind objects to determine wind-loaded aspects. Once you know which way the wind was blowing, look for smooth “pillow-like” piles of snow that appear “fat” or feel stiffer compared to the surrounding snow to identify Wind Slabs. Using small test slopes or uptrack tests as you travel can give you clues about how wind-drifted snow is reacting to your weight as a traveler. As you ascend in elevation, you’ll likely need to manage Wind Slabs on more specific terrain features such as confined gullies and convex rollovers. As you reach the alpine, the distribution may expand to more open slopes over 35 degrees where the possibility of triggering an avalanche increases.
(3/3/2023)
A skier triggered slab in the Alpental Valley on 3/3 that failed on a layer of graupel. This slab stepped down to the deeper 2/25 interface.
Photo: Aaron Richards