Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1.5–3
Weak layers in the lower portion of the snowpack exist and can been seen widespread at all elevations. Rain crusts from December are mixed between facets that were weakened from last week’s arctic cold front. Even though these layers are not consistently proving they can propagate and fail, the consequence of triggering an avalanche on any one of these weak layers would be very dangerous. The upper snowpack has taken on weight from rain and moisture and has the potential to overload a deeper weak layer if triggered. As you gain elevation to where temperatures have remained below freezing the wet slab problem will transition to the same persitant weak layer problems we have been talking about for weeks. The snowpack is "healing" and gaining strength at upper elevations where the temperatures are more moderate but have remained below freezing, but should be treated with caution until proven safe. Careful route planning and being mindful of what slopes you expose yourself to will be important for avoiding this low probability, and high consequence dangerous avalanche.