Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
The winds were cranking all around the West South as we said goodbye to the atmospheric river event on Tuesday night. Wind speeds over 100 mph were captured at multiple of NWAC’s weather stations around the zone, while others “only” made it to 80 or 90mph. These winds were certainly strong enough to transport any cold and dry snow onto leeward slopes or toward the sides of gullies and bases of cliffs to form dangerous Wind Slabs. The main problem these winds may have had was finding cold dry snow to transport. You’ll have to look to upper elevations above the rain/snow line to find this snow, and subsequently find Wind Slabs. We have some uncertainty around what elevation this transition takes place at, and it may be different depending on where you are in the zone, but it does exist. When you find it, you’ll know immediately and you should be on the lookout for wind-textured snow surfaces, freshly built cornices, and smooth pillow-like piles of snow to help you identify wind-loaded slopes that you should avoid.
(1/12/2021) This Storm Slab (D2) naturally triggered on 1/12 at Crystal Mountain. Wind Slabs could act similarly on Thursday on leeward slopes near ridgelines above the rain/snow line.