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Avalanche Forecast

Archived

Dec 21st, 2020–Dec 22nd, 2020

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

40 to 60 cm of snow now rests on a sketchy layer of surface hoar which has recently shown a propensity for connecting big pieces of terrain resulting in large avalanches, take a look at this example. It's time to seek out simple supported terrain that is not in avalanche paths.

Confidence

Low - Uncertainty is due to the limited number of field observations. Uncertainty is due to extremely variable snowpack conditions reported through the region.

Weather Forecast

Looks like we’re moving into a bit of a clearing trend this week.

MONDAY NIGHT: Freezing level at valley bottom, moderate NE wind, trace of snow expected.

TUESDAY: Scattered cloud cover, freezing level at valley bottom, light northerly wind, no significant precipitation expected.

WEDNESDAY: Scattered cloud cover, freezing level at valley bottom, light southwest wind, no new snow expected.

THURSDAY: Scattered cloud cover, freezing level at valley bottom with potential for a light alpine temperature inversion, light southerly wind, no new snow expected.

Avalanche Summary

There was a smattering of reported natural and human triggered avalanches on Saturday throughout the region with humbling photos of large avalanches. The MIN posts from the weekend really tell the story, you can view them all here. This observation from Sunday on a north facing slope looks to be failing on the mid December surface hoar.

Snowpack Summary

A steady stream of storms has resulted in 30 to 65 cm of light density new snow across the region with areas to the east around Blue River getting the larger amounts. Southwest winds have built slabs in lee features at upper elevations.

A spooky and active weak layer is now down 40 to 70 cm below the surface. In some areas it's a crust, in others it's surface hoar, and it may be surface hoar on top of a crust in some zones. The bond at this interface is poor and avalanches have recently failed on this interface throughout the region. 

Near the base of the snowpack is a crust that was buried in early November. This crust likely has weak facets associated with it. There have been no recent avalanches reported on this layer, though it may be possible to trigger from shallow, rocky terrain.

Terrain and Travel

  • Avoid freshly wind loaded terrain features.
  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Use careful route-finding and stick to moderate slope angles with low consequences.

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.