Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
Drifting of the new snow by strong southerly winds created 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. You could trigger a wind slab avalanche on steep slopes mainly on the north half of the compass 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.
- Soft slab avalanches of new snow are possible on slopes steeper than 30 degrees.
- 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.