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Avalanche Forecast

Archived

Dec 5th, 2020–Dec 6th, 2020

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 unlikely, human triggered possible.

Regions

Cariboos.

Temperatures are forecast to remain elevated in the northeast part of the region. Watch for signs of instability like pinwheeling in moist or wet snow.

As temperatures drop below freezing, avalanche hazard will decrease. Make observations and evaluate conditions as you travel.

Confidence

Low - Uncertainty is due to the limited number of field observations.

Weather Forecast

Saturday night: Clear, light to moderate southwest wind, temperature inversion breaking down, freezing level 500 m in most areas, remaining elevated at 2000 m in the northeast of the region.

Sunday: Increasing cloud, light to moderate southwest wind, freezing level 1100 m, 2000 m in the northeast of the region.

Monday: 10-20 cm new snow, moderate to strong south wind, freezing level 1000-1300 m.

Tuesday: 5-10 cm new snow then clearing, wind easing to light southwest, freezing level 1300 m.

Avalanche Summary

Loose wet avalanches size 1-2 likely occurred during the warmup on Wednesday and Saturday.

Our eyes and ears in the mountains are limited this winter due to fewer professional observations. If you go out in the mountains, please share your observations on the Mountain Information Network (MIN). Photos are especially helpful! Thank you so much for all the great MINs submitted so far! 

Snowpack Summary

A melt-freeze crust on steep solar aspects at treeline and above will soften through the day. On shadier aspects, alpine surfaces are predominantly wind affected, with soft snow still to be found in at lower elevations. Widespread growth of large surface hoar crystals (up to 2 cm!) and surface faceting have been reported. These types of crystals (crust, hoar, facets) that develop on the surface as it sits exposed during prolonged periods of high pressure like this often become a problem once buried by the next snowfall.

The lower snowpack is characterized by a couple of crusts, the most notable of which is sitting near the base of the snowpack, likely surrounded by a weak layer of sugary facets. It is most likely to be reactive to human triggers on south facing slopes and in shallow, rocky areas in the alpine.

Terrain and Travel

  • Start on smaller terrain features and gather information before committing to bigger terrain.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • Watch for unstable snow on specific terrain features, especially when the snow is moist or wet.

Problems

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.