Avalanche Forecast

Issued: Dec 13th, 2020 4:00PM

The alpine rating is moderate, the treeline rating is moderate, and the below treeline rating is low. Known problems include Persistent Slabs.

Avalanche Canada shorton, Avalanche Canada

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The main concern is the bond of recent snow to buried weak layers, especially around Blue River and Valemount where these layers are buried deeper.

 

Summary

Confidence

Moderate - Recent weather patterns have resulted in a high degree of snowpack variability within the region. Uncertainty is due to the limited number of field observations.

Weather Forecast

A weak frontal system arrives on Tuesday.

SUNDAY NIGHT: A trace of snow overnight, moderate southwest wind, low temperatures around -10 C.

MONDAY: Cloudy with some light flurries, moderate southwest wind, high temperatures around -8 C.

TUESDAY: Light flurries with up to 5 cm of new snow, strong south wind, high temperatures around -6 C.

WEDNESDAY: Another 5 cm overnight then clearing in the afternoon, moderate southwest wind, high temperatures around -6 C.

Avalanche Summary

Several large natural avalanches were recently reported at Chappel Creek (see this MIN report). These avalanches occurred on south aspects at treeline elevations. Based on the depth of these avalanches, they likely failed on recently buried surface hoar and/or sun crust layers. These photos suggest a persistent slab avalanche problem may exist, but we are uncertain about the details of this problem. Extra caution should be taken on steep treeline terrain around Blue River and Valemount where there may be enough snow above this weak layer to produce dangerous avalanches.

Otherwise some small wind slab and dry loose avalanches have recently been observed in alpine terrain.

Snowpack Summary

The alpine is wind-affected and lower elevations are capped by a hard rain crust. Reports suggest this crust extends up to anywhere from 1200 m to 1700 m. Sheltered areas at treeline likely have 15-40 cm of low density snow.

The main concern (and uncertainty) is whether this recent snow is bonding to a surface hoar layer and/or sun crusts. In most areas this snow has probably not developed into a concerning slab, with the exception of the Blue River and Valemount areas where there has been more snowfall. The most likely terrain for this problem is around treeline elevations where the snowpack has not been affected by wind or rain (see some good examples in these MIN photos).

 A buried rain crust can be found in the lower snowpack (50-100 cm deep) with some reports of weak snow around this crust. While we have not seen recent avalanches on this layer, it continues to produce occasional results in snowpack tests. It may 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.
  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.
  • Use caution on large alpine slopes, especially around thin areas that may propagate to deeper instabilities.

Problems

Persistent Slabs

An icon showing Persistent Slabs

Recent snow may sit above a layer of surface hoar and/or sun crusts at alpine and treeline elevations. This problem is most concerning around Blue River and Valemount where this layer is roughly 30 cm deep.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

1 - 2

Valid until: Dec 14th, 2020 4:00PM