Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
As water creeps deeper into the snowpack, widely propagating slabs may become possible. Buried layers of small facets, surface hoar, and larger facets near the ground could all act as the weak layer for destructive wet slab avalanches. You may be able to trigger wet loose slides that entrain deeper snow and become large as well. In many areas, you might just find challenging travel with deep mushy snow, a breakable crust, or a stout and slick rain crust.
The current conditions are a bit unusual, and wet slabs are tricky to predict, so give yourself an extra margin of safety with your travels. This means steering well out from underneath large, steep slopes while the snowpack adjusts. Look for recent avalanche activity as the number one bullseye of instability information. Wet, mushy, and unsupportable snow are also good indicators that wet avalanches are possible.
The same layers that we were previously concerned about with persistent slabs are concerning for wet slabs. See Willie's video below for a great example of this.
Example of a very large, wet avalanche.
Photo: Andy Harrington