Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Friday's storm brought 20-28" of snow (1.8-2.3" of SWE) to this zone. Snowfall was accompanied by strong winds blowing out of the SE-S-SW. This combination built very large, dense, 1-3 foot thick wind slabs on many slopes. Triggering a wind slab avalanche large enough to bury you remains likely today.
Wind slabs will be largest and most broadly distributed in upper and middle elevation terrain. Wind slabs commonly form along ridgelines and near mid-slope terrain features like ribs and gullies. Large slabs also build at the base of large cliffs and on aprons below couloirs during storms, a common occurrence in the Sawtooths.
Wind slabs and cornices that fail can be very effective triggers for the enormous, destructive persistent slab avalanches described below in Problem 2.
(3/11/2023) These avalacnhes failed in heavily wind-loaded terrain in the Boulder Mountains. They failed on a SE-facing slope at 9,600'. Note the obvious dunes visible in the snow surface above the crown.