Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
While fresh snow will create the potential for increased avalanche danger, wind should be the factor that determines the size and likelihood of the most consequential avalanches you encounter. Blowing or drifting snow, scoured snow surfaces on windward slopes, and stiffer, pillowy-looking drifts are all signs that wind slabs lurk nearby. Look for and simply avoid steep terrain where you see signs of active wind or recent wind loading.
You might also find unstable snow in wind-sheltered terrain, especially in areas that receive about 1’ or more of new snow or during periods of heavy snowfall. The old surface of crust, firm wind slab, or weak snow should have a poor bond with the cold and dry new snow above. Any avalanche you trigger may travel farther than expected. With continued thin snowpack conditions, avalanche risk will depend as much on the terrain in the runout as the size of the actual avalanche.
An example of early-season wind loading. Ground cover is visible in scoured areas while thick slabs form from wind loading.