Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
The first wind slab avalanche of the season was intentionally triggered on Dec 1 on the east face of Mt. Judah near Donner Summit (more info). Additional snowfall and SW wind over the past 24 hours has kept this avalanche problem ongoing with additional drifting and snow surface cracking observed yesterday.
In some areas, wind slabs may exist on top of a very weak, sugary (faceted) snowpack. Triggering lower on the slope than is common for a wind slab avalanche could easily occur anywhere a slab exists on top of weak faceted snow and the avalanche could fail wider than expected. In some areas, an easily missed, thin layer of faceted snow exists sandwiched between the recent new snow and a firm rain crust below it.
Use clues such as visible drifting snow, cornice formations, wind pillows, or other signs of snow distribution on the ground to identify areas that hold wind slabs. Exercise increased caution around areas where wind drifted snow has been deposited.