Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Fresh snow is adding fuel for continued wind transport at higher elevations. Winds have shifted from the north to west and are forming wind slabs on the lee sides of ridgelines and cross-loaded terrain features. In some areas, wind slabs are forming over a notably weak interface and will be easy to trigger or could entrain additional loose snow as they run downslope. Most slabs are relatively small; slopes with large fetches or in long-running terrain could be large. Look for evidence of recent drifting to identify the problem. Wind slabs will feel thicker and denser and have a smooth, rounded appearance. You can avoid the problem by traveling in wind-protected or wind-eroded terrain.
Natural wind slab avalanches on a cross drifted slope in Redwell Basin that ran around 1/7. More snow and more wind today means more avalanches like this.