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Avalanche Forecast

Archived

Feb 5th, 2020–Feb 6th, 2020

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

Regions

Purcells.

Wind slabs at upper elevations remain a concern. Seek out soft snow sheltered from recent winds.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Wednesday night: Cloudy, isolated flurries with a trace of snow, light to moderate northwest winds, alpine temperature -11 C.

Thursday: Mostly cloudy, scattered flurries with a trace of snow, light northwest winds, alpine high temperature -6 C.

Friday: Partly cloudy, isolated flurries with a trace of snow, light variable winds, alpine high temperature -5 C. 

Saturday: Cloudy, 5-15 cm of snow, light northeast winds, alpine high temperature -5 C. 

Avalanche Summary

Since the weekend storm, there have been several reports of failing cornices and small wind slabs. See this MIN report for a helpful illustration. Explosive triggers have also released several large avalanches breaking on deeply buried weak layers on a variety of aspects above 2200 m. This activity is a good reminder that this layer remains a problem in the region. Easier-to-trigger wind slab avalanches or cornice fall may have the potential to step-down to this layer.

During the weekend storm, numerous size 2-3.5 slab avalanches released naturally. A few were thought to have stepped down to deeper layers. These avalanches primarily occurred on leeward aspects at treeline and alpine elevations. Below tree line, wet loose avalanches ran naturally during the warm temperatures on Saturday. 

Snowpack Summary

Incremental snow and wind is adding to previous wind-loading in the alpine and at treeline. Where the snow is being drifted and stiffened by wind, human-triggered avalanches may be possible. Cornices are large and looming and may be reaching their breaking point.

40-60 cm of snow fell during the weekend storm above 1900 m. Extreme winds originating from the southwest and shifting to the northwest created a tricky loading pattern at treeline and above and accelerated cornice growth. 

Below 1900 m, 10-20 cm snow may cover a crust that formed during the storm from warm temperatures and rain. The snow above this crust is well-bonded and gaining strength.  

A weak layer of surface hoar may still be found about 90 cm deep around Golden and Kimberley, 50 cm deep around Invermere, and 130 cm deep along Kootenay Lake. As usual for the Purcells, the base of the snowpack contains basal facets. It remains possible to trigger these deep weak layers in shallow rocky start zones or from a heavy trigger such as a cornice fall. 

Terrain and Travel

  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • Seek out wind sheltered terrain below treeline where you can avoid wind slabs and find great riding.
  • Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.