Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
As has been the case for several weeks now, wind drifted snow continues to be our primary concern. Deep drifts from the last storm event have formed on the lee sides of ridge crests and terrain features on slopes facing NW-N-E. These drifts will primarily be found in upper elevation terrain though some exposed mid elevation slopes are also susceptible. At the highest elevations, a shift in wind direction has also deposited shallower, and more isolated drifts on to southerly aspects. Though gaining strength, I think human triggered avalanches up to 3' deep remain likely on steep, wind drifted slopes. A triggered wind drift also has the potential to step down into a buried, persistent weak layer causing a deeper, and even more dangerous avalanche.