Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
The Tetons received around 10 inches of snow water equivalent during the last storm cycle. Very strong southwesterly to westerly ridgetop winds accompanied this snowfall, and dense wind slabs formed at the mid and upper elevations. These slabs could fail on density breaks or graupel layers within the recent snowfall. Faceted snow from January can also be found in some areas. This scenario results in slab depths ranging anywhere from six inches to four or five feet. Daytime warming will increase the likelihood of triggering these slides, and natural activity could become possible in the afternoon.