Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
New snow instabilities will range from loose, long-running sluffs on old-firm surfaces to denser, shallow slabs where wind has built drifts of snow.
Expect to find pockets of instability near ridgelines, convex rolls, or on the sides of steep gullies. The size and likelihood of triggering a slide will increase as you climb in elevation into more wind-favoring terrain. Watch for signs of wind loading, like drifting snow, or snow blowing off ridgelines or peaks. Wind slabs may not always present as stiff or hollow-sounding slabs of snow; you may only encounter drifts of soft snow. Snowpack cracking or collapsing are clues that you have found this problem.
New snow fell on a variety of surfaces, including old sun crusts, wind crusts, and near-surface facets. Avalanches could break wider than you expect, where these slides fail on old snow below.