Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Modest amounts of new snow in the forecast shouldn’t add much to avalanche danger on their own. Adding wind to the picture is another story. At mid elevations, the only snow available for transport should be what falls after rainfall switches to snow early in the morning. Slabs at those elevations might be reactive, but not very big. At upper elevations, colder temperatures have kept the snow surface drier, allowing it to drift more easily and for wind slabs to grow thicker.
Monitor changes in new snow depth and stiffness as you gain elevation or switch aspects. Test slopes and hand pits can help you gauge the bond of new wind slab layers, but the safest bet is to avoid steep slopes on the receiving end of blowing and drifting snow.
An added complication is that a small wind slab avalanche could trigger a larger slab failing on older weak layers buried deeper in the snowpack. Canyon Creek and other areas north of Highway 542 are most likely where this is an issue, but less-traveled terrain could have a similar setup.
(4/9/2022)
Stiff, slabby snow? Check. Cracking? Check. Wind-affected surface? Congratulations, you found a wind slab!
Photo: Dallas Glass