Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
In addition to the Wind Slabs formed on Friday night and Saturday, you could find that some fresh slabs have developed by Sunday morning due to continued East winds at the Pass. Specific terrain features such as convex rollovers, the base of cliffs, or the sides of rock gullies will be the most likely location for these unstable pockets of snow to form. Of course, they are also prone to develop on the leeward side of ridgelines. These slabs could exist on aspects where you’re not used to seeing them, so keep a keen eye. Your number one indicator of Wind Slab formation should continue to be actively blowing snow. You can also look for fresh cornices and drifts, or large pillow-like piles of snow to help you identify areas to avoid. If you are traveling in snow that is firm or has a textured surface, you are likely already in wind-affected terrain.
(12/3/2022)
Actively blowing snow, freshly building sharp cornices, and textured surfaces. All easy to identify signs of wind-loading. Look for slabs to develop on the slopes on the left side of the picture.
Photo: Dallas Glass