Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
You can trigger large avalanches on leeward, wind-exposed slopes. Strong southwest winds transported snow and formed slabs on Tuesday night into Wednesday. Avalanches will be larger and easier to trigger above treeline. Signs of wind slab instabilities are shooting cracks, whumphing collapses, and recent slab avalanches on leeward and cross-loaded slopes. Stay off of slopes steeper than 35 degrees where you find deeply drifted snow, wind features, and overhead cornices. Cornices may be large and easy to trigger. If you do get up onto a ridgeline, give these a wide berth as they could break and trigger avalanches below.
In addition to slabs on the surface, deeper weak layers exist above 5,000ft in areas with a shallow snowpack, such as the Wenatchee Mountains. While it seems unlikely that you could trigger a persistent slab avalanche, we still have uncertainty at upper elevations. If you are in areas with less than 4 feet of snow on the ground, be prepared to make your own assessment of the snowpack.
Example of intense wind loading off a ridgeline.