Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1–2
Wind slabs are more likely in areas closer to the crest or a mountain gap where easterly winds were stronger on Saturday. Due to the atypical wind direction, slabs may have formed on different aspects than you’re used to. There also likely will be more mid-slope cross-loading. Visual clues such as fresh cornices, drifts behind objects, or textured surfaces can help you identify where the problem exists. They like to form near the base of cliffs, in confined chutes/gullies, or on the leeward side of ridgelines. Slabs should be larger and more reactive as you ascend in elevation or further south in the zone where the storm continued throughout Saturday.
Feel for density changes in the snow as you travel to help identify older wind slabs that may not be healing as quickly in these cold temperatures.
(1/11/2024)
Small, remotely triggered slab avalanche at White Pass.
Photo: Dallas Glass