Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind slabs from the recent storm may have formed over weak snow grains in alpine areas on northerly aspects. Forecaster, Matt Primomo, found this weak structure in the Icicle Creek drainage on Wednesday at around 6700ft. While the storm snow didn't seem reactive in wind-sheltered terrain, wind-loaded lee aspects with thicker slabs could potentially produce large avalanches. Use visual clues such as cornice formations and surface texture to identify wind-affected terrain. Also, consider sticking to wind-sheltered areas or lower angle slopes in high elevation, northerly terrain.
Look for signs of instability such as shooting cracks, collapsing, or recent avalanche activity. These are all bullseye signs of an unstable slope. You can also dig down quickly to observe if the snow slides easily off the crust and look for weak snow above the crust. If the snow easily slides on the crust, you find it weak snow, or see other signs of instability stick to conservative terrain with lower angle slopes.
(3/16/2022)
Wind slab in high elevation terrain in the Icicle Creek drainage.
Photo: Matt Primomo