Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
Yesterday, we observed wet slab avalanches in the Pioneer Mountains (see photos above/right). Expect this avalanche activity to continue as another weak overnight freeze and continued sunny, warm weather combine to send meltwater deep into the snowpack. The snowpack in this zone is very weak and faceted, particularly on slopes that face the northern half of the compass. Avalanches may occur when meltwater weakens these facets either in a weak layer within the snowpack or near the ground.
Wet slab avalanches are almost impossible to accurately forecast on a slope scale and the resulting slides often wipe out much of the season's snowpack. The best way to manage this problem is to avoid steep slopes with soggy snow. If the snow surface begins to resemble mashed potatoes or if you're punching through crusts that were supporting you early in the day, move to slopes with cooler, drier snow or call it a day.
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 is a great example. These slides can be triggered remotely—from a distance above, below, or to the side of a steeper slope. This problem is most likely along the northern edge of this zone. Read the persistent slab problem discussion here for more details.