Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Wind slabs may be present on Wednesday on leeward slopes, at the base of cliffs, or on the sides of gullies at middle and upper elevations. These slabs should reach peak instability in the morning hours and may increase in size and reactivity as you ascend in elevation. Textured snow surfaces or pillow-like piles of snow are signs that can help to identify potential wind loaded areas for you to avoid. Hand-pits and small test slopes can give an indication of how the new snow is bonding to the old snow surface. If you find a poor bond or experience clues of unstable snow such as shooting cracks or whumpfing collapses as you travel, steer around wind-loaded terrain.
Blowing snow, firm and textured snow, and cornice formation are all evidence that wind slabs are likely to be forming on lee slopes.