Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
There's still a chance of triggering a small, isolated wind slab in upper elevation terrain. We've only received bits and spurts of snowfall over the past 2 months, but there's been plenty of wind. Each wind event creates fresh pockets of drifted snow—some of which are sitting on weak layers formed during the mid-winter drought. A handful of natural wind slab avalanches occurred after the wet and windy storm earlier in the week, including one larger slide in the Smoky Mountains (report).
On Wednesday, I was with a professional avalanche course sledding in Pole Creek. Once we broke out into open, upper elevation terrain, the effect of recent and past wind events was readily apparent. Slope cuts on a small, safe test slope produced shooting cracks up to 10' long (photo above/right). We found multiple layers of wind-blown snow atop weak, sugary facets.
This is not a widespread problem, nor is it likely to produce large avalanches, but think about the consequences of taking a ride in a small avalanche before committing to a slope. If you find yourself in the wind slab's natural habitat—upper elevation, wind-exposed terrain—be on the lookout for evidence of windblown such as stiffer snow, drifted pillows, and dunes. Cracks shooting out from your board and sled are bullseye evidence of having found a sensitive wind slab.
(3/2/2022) On Wednesday in Pole Cr, slope cuts on a small test slope (9400', N) produced cracks up 10' long. The 10-12" thick slab consisted of multiple layers of wind-transported snow atop weak facets.