Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 2
Drifting of the new snow by southerly winds will create wind slabs on the lee side of major ridges and in and around terrain features like sub ridges, gully walls, mid-slope roll-overs, and under cliff bands. In some areas, these may fail naturally and/or will likely be easy for people to trigger, and even small avalanches of stiffer, wind-drifted snow could run fast and far on the slick crust formed during last week's warm temperatures.
- Avoid recent drifts or wind slabs on steep slopes. Wind slabs are made up of stiffer, redeposited snow that may be more supportable than the surrounding powder. Lense-shaped drifts often make hollow, drum-like sounds.
- Cracking is an obvious sign of wind slab instability.
- Shallow loose and soft slab avalanches of heavy new snow are also possible on steep slopes across the zone.
- An outlier at this point - hard slab avalanches failing on a buried persistent weak layer could be large and life-threatening. The weak, faceted snow that plagued the range in January is basically in the rear-view mirror but remains on the edges of our radar as we continue to find increasingly stubborn instability in our snow pit tests in areas with a shallower snowpack. Of note, red flags may not be present when avalanches failing on a persistent weak layer occur.