Avalanche Forecast

Issued: Jan 22nd, 2016 8:25AM

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

Avalanche Canada bcorrigan, Avalanche Canada

Wind slabs may be rider triggered and could be surprisingly large.

Summary

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

Light flurries are forecast for the next few days of day of the forecast period, ending late Sunday afternoon.  Strong southwest ridge top winds should become light to moderate by Sunday afternoon. Freezing levels will drop to valley bottom Sunday night, then rise again to1200m on Monday during the day.

Avalanche Summary

In recent days, several natural wind slab avalanches to size 1.5 were observed in high elevation terrain in the Elk Valley North area, as well as east of the divide.  A size 1 persistent slab avalanche was also noted on a steep cut bank below treeline. Although observations were limited at the time of publishing this bulletin, strong winds on Thursday and Friday will likely produce a new round of wind slab activity. In areas where buried persistent weak layers exist, wind-deposited snow will also add to the likelihood and consequences of triggering the overlying slab.

Snowpack Summary

Recent snows form earlier in the week with strong southwest winds  have been redistributed into wind slabs in higher elevation lee terrain. East of Crowsnest Pass new snow will overlie mainly scoured surfaces or hard stubborn wind slabs from last week. In general, the mid and lower snowpack are strong and well-settled in these areas.In areas to the west of the divide you're likely to find a mix of persistent weak crystals around 30cm below the surface. These crystals, which formed at the beginning of January, seem most reactive in open areas below treeline and consist of surface hoar, facets and a hard crust that formed on steep solar aspects. Additional snow load will add to the size and reactivity of this developing persistent slab. About 50cm below the surface you may also find a surface hoar layer which formed in December. Although no avalanches have been reported on this layer, it continues to produce sudden planar results in snowpack tests and may come to life with a large trigger or additional storm loading.

Problems

Wind Slabs

An icon showing Wind Slabs
Strong southwest winds on have redistributed loose surface snow into reactive wind slabs in exposed lee terrain. Hard wind slabs may promote surprisingly wide propagations.
Stay off recent wind loaded areas until the slope has had a chance to stabilize.>Be aware of the potential for wide propagations due to the presence of hard windslabs.>

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

Elevations: Alpine, Treeline.

Likelihood

Likely

Expected Size

1 - 3

Persistent Slabs

An icon showing Persistent Slabs
Up to 30cm of cohesive storm snow overlies a mix of weak crystals which seem most reactive, especially at and below treeline elevations west of the divide. Watch for triggering in steep open glades and in cut blocks.
Use extra caution on open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.>

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible - Likely

Expected Size

1 - 2

Valid until: Jan 23rd, 2016 2:00PM

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