Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
This is a return to our typical winter type of avalanche conditions. Signifcant snowfall overnight combined with moderate westerly winds will build wind slabs on lee slopes. Isolated terrain features may accumilate enough wind blown snow to produce large avalanches. Wind slabs are most sensitive to triggering during the storm and just after the storm. Use careful evaluation to determine which slopes have become wind loaded and monitor the depth of wind deposited snow. As wind slabs become deeper, avalanches can become larger. Wind slabs typically form below ridge tops, high points, and other features that catch wind transported snow. You can also find 'cross loaded' slopes where wind wraps around features. Signs of unstable snow such as recent avalanches and cracking in the surface slab are good indicators that you can trigger an avalanche.
Areas with sparse or dead trees can be subject to wind blowing snow. Watch for signs of wind slabs forming in these areas that you would typically think of as 'below treeline'.
Archive photo:
Cracking in fresh wind slab. This is a classic example of unstable snow.