Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Likely
- Dimensione
- 1–2.5
Yesterday's snowfall tapered off in the early morning and was followed by a significant southwest wind event that lasted until late last night. With abundant soft snow available for wind transport you can expect heavy dense slabs to have formed in leeward avalanche paths. Because winds decreased overnight the top layer of snow may not be cohesive and may disguise wind slabs immediately below the surface. Be alert for signs of instability such as shooting cracks and audible slope collapses. Large drifts, recent cornice growth, hollow upside-down feeling snow, and uneven snow surfaces are all clues that indicate nearby wind slabs. Do your own localized assessments and carefully evaluate terrain features that encourage drifting, such as the leeward sides of ridgelines, alpine couloirs, gully features, and cross-loaded depressions. While wind slabs may not react to the weight of a rider in all areas, the consequences of a large wind slab avalanche today could be high.
Wind transport of recent snow on 4/5/24. Photo: Steve Mace