Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Likely
- Taille
- 1–2
Precipitation rates will relax, but strong NW winds will continue to drift new snow and maintain reactive wind slabs in upper and possibly some middle elevation terrain. Look for these slabs to be thicker as you gain elevation into alpine terrain or as you approach the Cascade Crest, which received higher accumulations. These wind slabs have formed over crusts on most of the slopes and may fail within the new storm layers or on this crust that sits roughly 1-2 feet below the surface on wind-loaded slopes.
Look for these drifts to be most prevalent on the downwind sides of ridges and saddles, below cornices, and near rocky complex terrain. Blowing snow, wind-rippled surfaces, and sharp cornices are clear indicators that wind slabs may lurk on slopes nearby. Shooting cracks and recent avalanche activity are clear red flags to keep slope angles in check.