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Avalanche Forecast

Archived

Dec 26th, 2022–Dec 27th, 2022

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Kootenay Boundary, Bonnington, Grohman, Kootenay Pass, Norns, Rossland, Ymir, Moyie, St. Mary, Kokanee, Retallack, Valhalla.

Heavy snowfall, wind and warm temperatures have added to a weak snowpack where buried weak layers are primed for human triggering.

Confidence

Moderate

Avalanche Summary

A dramatic increase in avalanche activity was reported during Sunday. In the alpine numerous remotely trigger very large avalanches (size 2.5) have been reported. These were described as failing on the December 22nd facet interface/ Persistent weak layer on north east aspects with crown depths averaging 40 cm and gaining significant mass and running far upwards of 400 meters in length.

Past avalanche activity Friday reported several remote avalanches that were large (size 2). Wind loaded features stepped down to a persistent slab, failing on the December 22nd, December 17th or November 21st layers.

Read about their decision making after triggering the first avalanche here.

Snowpack Summary

The recent storm snow has warmed and become dense, forming slab like properties These wind and storm slabs have accumulated over layers of either facets, surface hoar or a crust. Westerly winds are redistributing snow into wind loaded features in treeline and alpine terrain.

The snowpack is becoming increasingly complex with several deeper instabilities that may persist through the season, and sustained past cold temperatures had continued to facet (weaken) the snowpack. Layers of concern in this snowpack:

  • The latest snowfall sits on a surface hoar layer from late December. Recent reports indicate the storm snow is very sensitive to human and remote triggers.

  • An early December layer of surface hoar in sheltered areas and a thin sun crust in open south-facing terrain is buried approximately 30-50 cm deep. This layer has recently produced surprising avalanches in upper treeline and lower alpine terrain features.

  • The most concerning layer buried in mid November is made up of large surface hoar crystals, facets, and a melt-freeze crust and can be found up to 80 cm deep. This layer has been reactive at treeline between 1700 to 2200 m, on all aspects.

Weather Summary

Monday Night

Heavy snowfall will continue with 10-15 cm expected overnight. Sustained moderate southwesterly wind 40 to 60 km/h . Alpine temperatures warming to or above -4°C as freezing levels maintain at 500 m.

Tuesday

Snowfall, heavy at times 15 to 30 cm. Freezing levels climb to 1500 m for a brief period near the end of the day. Moderate to strong southwest winds 60 to 70 km/h. At terrain below 1500m a potential for rain on snow is possible.

Wednesday

Snowfall, moderate 10 to 15 cm. Freezing levels will descend to near valley bottom by days end Moderate to light north winds 20 to 30 km/h.

Thursday

Snowfall, light with trace amounts. Freezing levels near valley bottom. Light southwest winds 20 to 30 km/h.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.