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Avalanche Forecast

Archived

Dec 12th, 2020–Dec 13th, 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, human triggered possible.
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

North Columbia.

Triggering avalanches is possible on slopes that have more than 30 cm of snow above crust and surface hoar layers.

 

Confidence

Moderate - Recent weather patterns have resulted in a high degree of snowpack variability within the region.

Weather Forecast

SATURDAY NIGHT: Partly cloudy, light west wind, low temperatures around -15 C.

SUNDAY: Cloudy with some light flurries in the afternoon, light southwest wind, high temperatures around -10 C.

MONDAY: Cloudy with up to 5 cm of new snow by the morning, light southwest wind, high temperatures around -8 C.

TUESDAY: Light flurries with 5-10 cm of snow, moderate southwest wind, high temperatures around -6 C.

Avalanche Summary

Over the past few days there have been a few reports of small avalanches above the recently buried surface hoar and crust layers. These include several dry loose avalanches in steep terrain and a few size 1 skier triggered avalanches in the Selkirks. The skier triggered avalanches were 30-40 cm thick (see the photo in this MIN report). While these avalanches have limited destructive potential, we anticipate this developing into a more concerning problem when more snow arrives.

Snowpack Summary

The storm earlier this week delivered a complex mix of snow, rain, and freezing rain. As a result the upper snow is highly variable. Several crusts have been reported including a widespread rain crust at lower elevations. In western and southern parts of the regions (e.g. the Monashees and Revelstoke area), this crust has been reported to extend into the alpine, with just a dusting of snow above the crust. Further east and north, temperatures remained colder during the storm and 20-40 cm of low density snow sits on the surface.

The primary concern right now is areas where this recent snow buried a widespread layer of surface hoar and/or sun crusts. This is most likely a problem in areas where 30+ cm of snow has fallen on this layer and less of a problem in areas with rain crusts near the surface. Overall, we suspect the most likely spot to find a slab above this weak layer is at treeline (and south-facing alpine) terrain in northern and eastern parts of the region.

Down near the ground remains a thick rain crust with sugary facets above and below from early November. While we have not seen recent avalanches on this layer, it produces occasional hard results in snowpack tests. It could be reactive to human triggers on shallow rocky slopes in the alpine or alpine-like features at treeline.

Terrain and Travel

  • Investigate the bond of the recent snow before committing to your line.
  • Look for signs of instability: whumphing, hollow sounds, shooting cracks, and recent avalanches.
  • Be careful with wind loaded pockets, especially near ridge crests and roll-overs.

Problems

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.