Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Wind Slab avalanches occurr when the wind moves soft snow from windward slopes (in this case Southwest and South) onto lee slopes (North and East in this case). The wind can pack this snow into a more cohesive slab. Wind Slabs most often occurr below ridglines and high points, or on the lee of mid slope ridges or features (when the wind is moving across a slope).
On Wednesday potential Wind Slabs will grow throughout the day as more snow falls into the afternoon and the wind increases. Several inches of new snow fell in some regions on Tuesday afternoon and will be available for transport. The forecast is calling for 2-3 more inches by Wednseday evening. When gauging the potential size of Wind Slab avalanches remember that wind deposited snow can be 3-5 times as deep as what has fallen in meadows or glades.