Avalanche Forecast

Issued: Dec 19th, 2018 4:41PM

The alpine rating is considerable, the treeline rating is considerable, and the below treeline rating is considerable. Known problems include Wind Slabs and Persistent Slabs.

Avalanche Canada dsaly, Avalanche Canada

Avalanche hazard will rise with incoming snow and increased winds. In areas that accumulate more than 30 cm snow, bump the avalanche danger to HIGH.

Summary

Confidence

Moderate - Intensity of incoming weather systems is uncertain.

Weather Forecast

WEDNESDAY NIGHT: Cloudy with isolated flurries, accumulation up to 5cm. Light to moderate south-southwest wind. Freezing level below 1000m. THURSDAY: Snow, 10-25cm new snow, increasing through the day. Moderate southwest wind with strong to extreme gusts. Freezing level rising to 1600m. FRIDAY: Mix of sun and cloud, isolated flurries. Light west wind with strong gusts. Freezing level valley bottom. SATURDAY: Mix of sun and cloud. Light west wind. Freezing level valley bottom.

Avalanche Summary

Extensive recent avalanche activity has occurred in the Purcells since December 12. Explosives and skier traffic are triggering large (size 2) avalanches, and although natural avalanche activity has started to subside, human-triggered avalanches remain a concern. Over the weekend, a small sluff triggered by a skier stepped down to a deeply buried weak layer (likely basal facets) causing a size 2 avalanche on Sunday. Another very notable avalanche occurred on Saturday when a size 2.5 avalanche was remotely triggered from 50-100m away on a northwest aspect at 2250m.

Snowpack Summary

Approximately 60-90 cm of recent snow sits on a weak layer of facets (sugary snow), surface hoar (feathery crystals), and a sun crust (on south facing slopes). Strong winds have promoted widespread slab formation, particularly with the most recent new snow available for transport. Another layer of surface hoar and sun crust is now buried 80-150 cm. The potential may exist for smaller avalanches to step down to this deeper layer, resulting in very large avalanches. The most likely areas for this layer to be a problem is where the surface hoar sits on the sun crust, which is most likely on steep south facing terrain at treeline. At the base of the snowpack is a crust that formed in late October. This layer is likely only a problem on large, steep alpine features with a shallow snowpack. It would likely take a large trigger, such as a cornice fall, to produce an avalanche on this layer.

Problems

Wind Slabs

An icon showing Wind Slabs
Wind has redistributed new snow and encouraged slab development in lee (downwind) areas.
Use caution in lee areas. Recent wind loading have created wind slabs.If triggered wind slabs may step down to deeper layers resulting in large avalanches.

Aspects: North, North East, East, West, North West.

Elevations: Alpine, Treeline.

Likelihood

Likely

Expected Size

1 - 2

Persistent Slabs

An icon showing Persistent Slabs
Snow accumulation from recent storms has buried a weak layer 60-120 cm deep. This weak layer consists of facets (sugary snow), surface hoar (feathery crystals), and sun crust. Wind loaded pockets areas could have over 200 cm on this layer.
Pay attention to overhead hazards like cornices which easily trigger persistent slabs.Use conservative route selection, choose moderate angled and supported terrain with low consequence.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Likely

Expected Size

1.5 - 3

Valid until: Dec 20th, 2018 2:00PM

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