Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind slabs will be most reactive where they overly surface hoar.
Large persistent slab avalanches have been occurring across the region, making low-angle, conservative terrain the best choice.
Wind slabs will be most reactive where they overly surface hoar.
Facets and/or surface hoar buried 40 to 80 cm deep are most prominent on north-facing slopes. Avoid areas with a thin or variable (thin to thick) snowpack.
Many size 2 to 3 persistent slab avalanches were reported on the Mountain Information Network over the weekend (see photos). This includes several slabs triggered by riders, including remotely. The AvCan field team observed some large natural slabs at Seaton that likely occurred on Monday.
Light snow and southerly winds continue to redistribute recent snowfall. This snow is accumulating on a layer of surface hoar buried 30 to 50 cm deep. This layer of surface hoar is present in the alpine and on aspects that are not exposed to sunlight.
Another layer of facets, surface hoar and/or a crust buried in mid-February is 40 to 80 cm below the snow surface and has been reactive in snowpack tests.
Deeper in the snowpack, a weak layer of facets and a crust from early December can be found. This layer appears to be dormant but is still worth keeping in mind in thin snowpack areas in the alpine.
Tuesday Night
Partly cloudy. 10 km/h south ridgetop wind. Treeline temperature -2 °C.
Wednesday
Mix of sun and cloud. 20 km/h southeast ridgetop wind. Treeline temperature -1 °C. Freezing level 1600 m.
Thursday
Mix of sun and cloud with 0 to 2 cm of snow. 40 km/h southeast ridgetop wind. Treeline temperature -3 °C. Freezing level 1200 m.
Friday
Mostly cloudy with 0 to 1 cm of snow. 40 km/h southeast ridgetop wind. Treeline temperature -6 °C.
More details can be found in the Mountain Weather Forecast.