Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Winds have redistributed the light, upslope snow fall that fell at higher elevations since early in the week. Winds reached hurricane force overnight from the west-northwest which typically builds firm wind slabs from 1F to P hardness. The most recent snowfall was very low density and transported easily so you are likely to encounter softer drifts at treeline and in protected areas. Harder slabs will exist in more wind exposed areas where snow has loaded into direct lee terrain features and crossloaded onto others. The larger, firmer slabs will be more stubborn to a human trigger but could be on the larger side if triggered (D2.5). Use the terrain to your advantage when travelling to avoid likely trigger points such as thin spots near the bottom edge and near rocks. Assess these slabs carefully for signs of instability such as cracking, collapsing or a drum-like surface that indicates softer, weaker snow beneath. Reduce your exposure to apron-shaped deposits of snow that accumulate below steep gullies and cliffs.. These have a history of growing large after wind events. Smaller and more reactive slabs may be tucked into more wind sheltered locations lower in the terrain and on steep, narrow drainages at mid elevations.
Softer wind slabs such as this may be found in areas not exposed to the higher wind speeds that occurred at higher elevations. Seek lower angled slopes if you see evidence of cracking like this.