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Avalanche Forecast

Archived

Feb 6th, 2021–Feb 7th, 2021

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

Regions

Kootenay Boundary.

A weak layer of surface hoar continues to produce large avalanches in response to human triggers around treeline. Stick to low angle slopes and treat open glades and leeward terrain features as suspect. 

Confidence

High -

Weather Forecast

Saturday night: Partly cloudy, moderate westerly ridgetop wind, alpine temperature -7.

Sunday: Mix of sun and cloud, light northwest ridgetop wind, alpine high -12.

Monday: Sunny, light to moderate northwest ridgetop wind, alpine high -17.

Tuesday: Sunny, light northerly ridgetop wind, alpine high -18.

Avalanche Summary

There have been numerous large natural, human and explosive triggered avalanches reported over the last couple of days. These include size 2-3 results from explosive work conducted Friday, as well as multiple size 2-3 avalanches remotely triggered by skiers on Thursday. Most of these avalanches failed on the recently buried persistent weak layer. Many occurred at elevations around treeline where the layer exists as surface hoar.

It is notable that a size 3.5 was reported to have failed on a crust that was buried in early December. A smaller avalanche stepped down to this deeper layer, resulting in a very large and destructive avalanche.

Snowpack Summary

30-60 cm of recent snow may sit on a weak layer which exists as a freezing rain crust in some areas and surface hoar in others.. It is not known how widespread this layer is, but it may have the potential to produce avalanches where it exists.

There is now about 50-80 cm of recent snow sitting above a widespread persistent weak layer that consists of facets in some areas, a melt-freeze crust in many areas, on a sun crust on steep south-facing slopes, and large surface hoar in sheltered areas. This layer has been the most reactive at treeline and below treeline, where it exists as surface hoar.

There are potentially several more layers of surface hoar in the upper snowpack, with the most notable one down about 80-120 cm. This layer was buried in early January. 

A crust surrounded by weak faceted grains is buried deep within the snowpack. It may be possible to trigger this layers with a large load.

Terrain and Travel

  • Use conservative route selection and resist venturing out into complex terrain.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Keep in mind that human triggering potential persists as natural avalanching tapers off.
  • Be careful as you transition into wind affected terrain.

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.

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.