Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Very Likely
- Dimensione
- 1–2
Wind-drifted snow accumulates more rapidly than direct snowfall alone and may form cohesive slabs of variable depth over weak surface snow. These will most likely be found on the leeward side of ridges and in cross-loaded gullies and couloirs. Watch out for changes in snow surface texture and hardness around terrain features that block or re-direct winds. Shooting cracks and firm hollow-sounding snow are signs that new wind slabs may be unstable in your area. Wind slabs may be touchy where they are poorly bonded to melt-freeze crusts and yesterday's weak snow surface. Extra caution is warranted around leeward start zones. When in doubt avoid wind-loaded slopes.
Large human-triggered wind slab in Redcone Bowl. 12/28/22.