Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Alternating wind events following the last storm created wind slabs on most aspects near and above the treeline. Slabs that formed from southwest winds during the storm on 2/5 have become stubborn and would need a large trigger like a cornice fall to release. Smaller and more sensitive wind slabs were created by NE winds on 2/6 and in the early hours yesterday (2/7). At upper elevations, be suspect of features that encourage drifting such as the leeward sides of corniced ridgelines, gully features, and cross-loaded depressions. You can track the extent of this problem by periodically assessing surface snow as you move through terrain. Check for the presence and depth of cohesive layers. Look for shooting cracks around terrain features that block or re-direct winds, especially when transitioning to steeper terrain. Triggering even a small slab may have higher consequences if the slope is above a terrain trap.