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Avalanche Forecast

Archived

Feb 26th, 2022–Feb 27th, 2022

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Purcells.

Watch for new wind slab formation on Sunday as new storm snow accumulates. Older wind slabs may also still be reactive to human-triggers.

Confidence

Moderate - Uncertainty is due to the speed, direction, or duration of the wind and its effect on the snowpack. Uncertainty is due to how buried persistent weak layers will react with the forecast incoming weather.

Weather Forecast

The first in a series of relatively weak storm systems is forecast to reach the region on Sunday morning.  

Saturday Night: Increasing cloud cover, light to moderate SW wind, treeline low around -10 °C. 

Sunday: Light snowfall 4-8 cm, moderate SW wind, treeline high around -4 °C. 

Sunday night and Monday: Light snowfall 10-15 cm, moderate SW wind, treeline high around -1 °C.

Monday night and Tuesday: Mainly light snowfall, moderate to strong SW wind, freezing levels reaching around 2000 m. 

Avalanche Summary

On Friday, a size 1 wind slab was remotely triggered from 3 m away on a north aspect in the alpine which was 10 cm thick. A size 1.5 wind slab was reported which was triggered on a south aspect and was 20 cm thick. Explosives triggered a couple cornices which triggered wind slabs on the slopes below. One other small avalanche was triggered on a sheltered roll at treeline which failed on the mid-February surface hoar. 

On Thursday, a few natural wind slabs up to size 2.5 were observed in the alpine in the western part of the region. Explosive use triggered several size 2-2.5 cornice releases. One of these cornices releases triggered a small slab on the slope below. 

Snowpack Summary

The new snow will bury a highly variable snow surface which includes wind-affected surface in exposed terrain, a thin sun crust on solar aspects which may be faceting, surface hoar in sheltered areas, and/or old storm snow which may be faceting on shaded slopes. 

A weak interface from mid-February was down around 20-40 cm prior to the storm. It consists of a sun crust on solar aspects, facets, and/or surface hoar. This layer was previously only reactive in wind-loaded terrain where a slab had formed but it is expected to become a more widespread problem as the storm progresses and builds a more widespread slab.

A layer of buried surface hoar from late-January sits 30-60 cm deep in the snowpack and is most likely to be found on north aspects in sheltered areas. Though there haven't been reports of recent avalanches on this layer in this region, it is still on the radar of many operations and could potentially wake up during the storm. 

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.