Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1
Strong SSW ridgetop winds yesterday created areas of blowing snow and enough wind loading to build small wind slabs near and above treeline on NW-N-NE aspects. Four small skier triggered avalanches were reported yesterday, at least two of which were intentionally triggered. In all cases avalanche size was too small to bury a person (more info below). Winds have shifted more to the S and snow on the ground available for wind transport is diminishing. Wind slabs are expected to be more difficult to trigger today than yesterday in the majority of areas. In isolated areas, triggering may remain easier today due to the presence of surface hoar, large stellar, and/or plate crystals at the weak layer interface. These are uncommon weak layers for this region and will make for more atypical remote triggering and delayed stabilization in any areas where they exist.
Terrain management to specifically avoid areas of recent wind loading is the wise choice today. Wind pillows, the leeward side of ridges where abrupt changes in snowpack depth occur, and below cornice features are simple ways to identify where unstable wind slabs might exist. More experienced travelers will be able to read micro terrain features, observe snow surface texture and feel slab over weak layer density changes to more precisely determine the boundaries of wind slabs.