Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Thursday’s wind event had unequal outcomes for the west slopes with some areas seeing minimal wind effect while terrain a ridge away got hammered. Natural and human triggered slabs were mostly limited to D1 in size but a few were larger. Some observers definitely backed off of steep convex terrain holding fresh wind slab. Alpine terrain generally saw more wind but some high peaks were spared. Wind affected snow and fresh slabs are probably more readily found the farther east you travel towards the Cascade Crest.
Wind slabs will probably have a similar, scattered distribution Friday. Evaluate slopes on a case-by-case basis as some commonly loaded slopes could be slab-free while others will be a no-go. Wind slabs may be easier to trigger where they formed over a crust on solar aspects.
Cornices and other clues that show the usual direction of wind loading - normally from the south and west - might not be useful to determine where fresh wind slab lurks. Instead look for recently scoured ridgelines with smooth, fat, or pillowy-looking drifts on the slope below. Test slopes and hand shears will help gauge wind slab reactivity and depth and can help you identify areas where they are easier to trigger.
(2/23/2023)
A skier was caught and carried in this small wind slab on Thursday. Crown visible in the narrow chute above tracks and debris.
Photo: Trevor Kostanich