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Avalanche Forecast

Archived

Feb 3rd, 2020–Feb 4th, 2020

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

Regions

Cariboos.

Avalanche hazard exists where the wind has loaded cornices and drifted recent snow into wind slabs. Give cornices a wide berth and assess for wind slab conditions before committing to terrain.

Confidence

Moderate - Uncertainty is due to how quickly the snowpack will recover and gain strength. Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Monday night: Clear, light northwest winds, alpine high temperature -18 C.

Tuesday: Increasing cloud, 5-15 cm of snow, strong southwest winds, alpine high temperature -10 C.

Wednesday: Cloudy, 10-20 cm of snow, moderate southwest winds with strong gusts, alpine high temperature -7 C, freezing level rising to 900 m.

Thursday: Cloudy, isolated flurries, light west winds, alpine high temperature -5 C.

Avalanche Summary

During the storm, numerous small to very large (size 1.5-4) avalanches released naturally in the new snow. These avalanches primarily occurred on leeward aspects at treeline and alpine elevations. Below tree line, wet loose avalanches were releasing naturally during the warm temperatures on Friday.

With continuous stormy weather over the past week, operators have reported three persistent slab avalanches that were both naturally and skier-remote triggered. These very large (size 2.5-4) avalanches were breaking 100-200 cm deep across a variety of aspects above 1900 m. Wind slab avalanches or cornice fall may have the potential to step-down to this layer.

Snowpack Summary

There have been substantial changes to the snowpack over the past few days. 40-60 cm of snow fell during the weekend storm above 1700 m. Higher snow totals fell in the southeastern parts of the region. Strong winds originating from the southwest and shifting to the northwest have created a tricky loading pattern near and above tree line and have elevated concern for cornice triggers. These winds have drifted the snow into stiff slabs on leeward terrain features that remain prone to human triggering. Check out this MIN report for a helpful illustration of these conditions. 

During a warming event Saturday night, rain saturated snow surfaces up to around 1700 m that have since formed a crust.

The mid and lower snowpack are generally well settled and strong, however there is a weak layer of surface hoar currently buried 70 to 150 cm deep. This layer has shown signs of instability in the region on slopes between 1700-2400 m. New snow, rain, and warming have added considerable strain to this weak layer, and it may require more time to adjust to the recent load.

Terrain and Travel

  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • 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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.