Wet Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–3
We're in the wet slab gray area of lowering probability, but high consequences. We're several days past the peak of a wet slab cycle, but we're not out of the woods yet. We might start getting the much-needed refreeze at the highest elevations, but temperatures remain uncomfortably mild at most NWAC forecast elevations. Two factors keep us on edge: (1) additional snowmelt with temperatures in the 30s and low 40s, along with patchy sunshine; and (2) recent rainwater working deeper into the snowpack. As water continues to seep deeper into the snowpack, it could pool on previous dry crust interfaces. This provides the lubrication necessary for a heavy, dense slab to release without warning. Wet slabs have a way of surprising novices and seasoned professionals alike. They can be triggered by a rider, cornice fall (we've seen multiple examples in the past 3 days), or the lubrication of a weaker interface above a crust. The long tail of potential slab release makes this problem really difficult to forecast.
To stay safe, continue to reduce your exposure to open slopes 35 degrees and steeper. Since a rogue natural avalanche remains possible, keep your eye to ensure there are no steep slopes above you. Recent wet avalanches serve as a reminder that a very large wet slab can run long distances on low angle or even flat terrain.
With water saturing the snowpack: Glide cracks can release off smooth bedrock slopes and may be large. You can also trigger smaller wet loose avalanches within the saturated snow near the surface on slopes steeper than 35 degrees.
(1/29/2024)
A natural wet slab in upper White River Canyon.
WS-N-R1-D1.5-U
Photo: Joseph Dellaporta