Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 2
New wind slabs have formed on wind-loaded slopes as a result of new snow and gale force winds. Near and above treeline NW-N-NE-E-SE aspects above 8000 ft where the most new snow has accumulated should hold the largest wind slabs. As snow levels drop today, additional snow and intense, pervasive winds will cause existing wind slabs to grow in size and new wind slabs to form at lower elevations and potentially in some below treeline areas. Large human-triggered wind slab avalanches remain very likely and natural wind slab avalanches are likely. In areas where rain falls on previously wind-loaded slopes, wind slab avalanches could involve wet snow and release more easily.