Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Newly developed wind drifts may be triggered in the mid and upper elevations and most prominent on steep northwest to northeast to southeast facing slopes. These drifts should be reactive to cornice drops and ski cuts but best left alone and avoided. Look for the smooth and rounded, scalloped appearance of any wind drifts. These should become more stubborn as the day wears on.
Side Note: some areas received a fair bit of graupel with the storm. This graupel can bounce downhill and pool beneath cliffbands or at significant slope angle transitions (from very steep to moderate) and remain sensitive to provocation briefly after a storm.