Wet Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 2–3
Wet slab avalanches are a problem to avoid, and they will begin to come into play today. Water from snowmelt will percolate down through the snowpack, wetting layers buried 1-3 feet deep that have been dry all year. The snowpack in this zone is very weak and faceted, particularly on slopes that face the northern half of the compass. The facets will behave unpredictably as they get wet for the first time. This process can result in wet slab avalanches that wipe out much of the season's snowpack. Wet slab avalanches can be triggered or release naturally. These types of slides are both deceptively powerful and almost impossible to accurately forecast on a slope scale.
Given the power of wet slabs and the difficulty associate with predicting exactly when and where they could release, we have to avoid steep slopes with soggy snowpacks. If the snow surface begins to resemble mashed potatoes, stick to gentler terrain or move to slopes with cooler, drier snow.
ADDITIONAL DISCUSSION:Persistent slab avalanches are possible on NW-N-NE aspects at middle and upper elevations. The natural avalanche Scott observed Tuesday on Bear Peak (photo to right/above) is a great example. The snow that fell in the past 2 weeks buried a snowpack consisting mostly of very weak, sugary faceted snow. These slides can be triggered remotely—from a distance above, below, or to the side of a steeper slope—or by smaller loose snow avalanches coming from above.