Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Tuesday's storm ended cold and convective with a lot of graupel, creating the potential for loose snow to run on steep slopes. However, the last storm was accompanied by plenty of wind and slabs lurk a few inches below the snow surface. While most of the slabs triggered by Mt Hood Meadows on Wednesday were stubborn and small, several were in the large range above the treeline. This size distribution should be the same on Thursday. Note any cracking under the less cohesive surface layer. Probe for punchy layers in the recent storm snow. And anticipate slab development on typical aspects even if you can't see them. When in doubt, stick to windward slopes, ridgelines, and avoid unsupported, lee slopes steeper than 35 degrees. If you are in an area with active wind transport or fresh, sharp cornices anticipate smaller, but more reactive slabs to develop in the immediate lee of ridgelines.
Example: Steep, wind-loaded features where you can trigger an avalanche on Thursday.
Photo: Paris Gore