Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2.5
Generous amounts of rain and continued meltwater have reached all the way through the snowpack, causing snow to lose cohesion and become quite unconsolidated. Facets that formed at the base of the snowpack and around the December rain crusts are saturated and lubricated, but haven't had an opportunity to refreeze and gain much stability yet. As temperatures go down to just around freezing today the chance of triggering a wet slab avalanche will gradually decrease, but won't be completely off the table. This problem will likely exist primarily on mid elevation slopes where precipitation from today will be more rain than snow.