Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2
Gale force wind will drift and deposit high intensity snowfall onto avalanche terrain near ridgetops, in gullies, and on open slopes, creating a wind slab avalanche problem. Slopes that are more filled in than surrounding areas with wind drifted snow are the main areas of hazard. Most slab avalanche potential will occur in above treeline and near treeline terrain today, but may extend below treeline to a lesser extent due to the strength of the winds.
Slopes below cornices and wind drifts are the main areas of concern, but consider any avalanche terrain that in rapidly filling in with wind drift snow as suspect. Snow surface cracking and/or fresh avalanches are indications of unstable snow in the immediate area. Consider avoiding any avalanche terrain where indications of potentially unstable wind slabs are present.
(1/1/2025) A car sized block of cornice broke off Wednesday afternoon, triggering a shallow wind slab avalanche. Expect avalanche size to increase today in this type of terrain.
NE aspect along the Sierra Crest to the south of Mt. Lincoln, Donner Summit area, CA