Avalanche Forecast

Issued: Jan 30th, 2016 8:56AM

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

Avalanche Canada triley, Avalanche Canada

Avalanche danger is decreasing due to cooling after the storm. The deeply buried persistent weak layer continues to be a concern for possible large avalanches.

Summary

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Unsettled with flurries overnight combined with moderate westerly winds and freezing levels down to valley bottoms. Continued overcast with light northwest winds and alpine temperatures around -14 on Sunday. Mostly sunny on Monday with light northwest winds and alpine temperatures around -15. Sunny with light winds and cool temperatures on Tuesday.

Avalanche Summary

No new observations on Saturday from this region. A natural cornice fall in the Lizard-Flathead region released size 2.5 on an east aspect with an approximate 2 metre fracture under the cornice. (this observation came in after I had published the Lizard-Flathead forecast, so it is not reported there).On Friday, our field team reported several natural avalanches up to size 3.0 on east aspects that were visible from Crown mountain in the Elk Valley North area. These avalanches probably started from wind loading or cornice falls. The interesting observation about these slides was that they stepped down in the track or at the fans around 1900 metres elevation and resulted in a larger avalanche than the initial release. This suggests that it is possible to trigger an avalanche in the run-out with the right load in the wrong place.

Snowpack Summary

I suspect that a supportive melt-freeze crust has developed below about 1600 metres due to the cooling trend and lower freezing levels. Recent strong to extreme winds developed storm slabs in the alpine and at treeline, and also resulted in new fragile cornice growth. The persistent weak layer of buried surface hoar was found down 45 cm at 1850 metres and down 90 cm at 2150 metres in the Crown mountain area, and compression tests gave hard sudden planar results. A weak crust/facet layer from early-December is typically down over 1m. It has become difficult to trigger this layer but it is still reactive in snowpack tests suggesting that if you are able to trigger it, the layer is capable of wide propagations and large destructive avalanches.

Problems

Storm Slabs

An icon showing Storm Slabs
Recent storm slabs and pockets of wind transported snow may continue to be triggered by light loads like skiers or riders. Natural cornice falls may trigger storm slabs in the path or track of the avalanche.
Use ridges or ribs to avoid pockets of wind loaded snow. >Be aware of the potential for wide propagations due to the presence of hard windslabs. >Avoid freshly wind loaded features. >

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible - Likely

Expected Size

1 - 3

Persistent Slabs

An icon showing Persistent Slabs
The persistent weak layer of buried surface hoar on the west side of the region and a buried crust/facet combination on the east side of the region continue to be a concern for human triggering, or from triggering by storm slab avalanches in motion.
Be aware of the potential for large, deep avalanches due to the presence of buried surface hoar.>

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible

Expected Size

3 - 5

Valid until: Jan 31st, 2016 2:00PM