Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind Slabs are formed when the wind blows snow across the terrain and this snow comes to rest on sheltered or lee slopes below ridgelines and behind crossloaded features. Wind transported snow can be 3-5 times as deep as the amount of snow that has fallen from the sky. The wind not only moves the snow; it also deforms the snow, breaking up the crystals so that they can pack tightly into a cohesive slab.
During the period of snowfall from Sunday through Monday we will experience shifting winds. On Sunday the wind was from the east, overnight it will be more southerly, and by Monday afternoon it will be from the southwest. Due to this shift and variations across terrain features, wind slabs are possible on all aspects. On Sunday morning there were observations from across the range of surface hoar. If this surface hoar remained intact as the new snow fell, it could create a particularly weak layer for wind slabs to fail on.