Avalanche Forecast
Issued: Dec 27th, 2020 4:00PM
The alpine rating is , the treeline rating is , and the below treeline rating is Known problems include Persistent Slabs, Wind Slabs and Deep Persistent Slabs.
JSmith,
Avalanche Canada
Multiple critical weak layers in the snowpack that could produce large avalanches remain possible to human trigger and are keeping the hazard elevated. A disciplined approach to decision making is needed to play safe.
Summary
Confidence
Low - Uncertainty is due to the limited number of field observations. Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.
Weather Forecast
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SUNDAY NIGHT: Cloudy / Light, west ridgetop wind / alpine low temperature -15 / Freezing level valley bottom.
MONDAY: Cloudy / Light, west ridgetop wind / alpine high temperature -9 / Freezing level valley bottom.
TUESDAY: Mostly sunny / Light, northwest ridgetop wind / alpine high temperature -11 / Freezing level valley bottom.
WEDNESDAY: Cloudy / Moderate, northwest ridgetop wind / alpine high temperature -11 / Freezing level valley bottom.
Avalanche Summary
On Saturday, a skier remotely triggered an avalanche on a southwest aspect below treeline, north of Kicking Horse Mountain Resort. No size was reported.
On Wednesday there was a report of a snowmobile triggered size 2 deep persistent slab avalanche in the north of the region. This MIN post highlights the avalanche and the current nature of the snowpack.
On Tuesday there were several reports of deep persistent slab avalanches running size 2-3 on southeast, east and northeast aspects. Three of these were size 2's triggered by skiers. Check out this MIN report from Tuesday afternoon for an example.Â
Snowpack Summary
Winds blowing from a variety of directions last week formed wind slabs in lee features at treeline and above.
There are currently several critical layers of concern. The early December surface hoar is down 30 to 80 cm. It has recently been sensitive to remote triggering which is well illustrated in this MIN post from the Golden area.
Below, or near the surface hoar you may encounter a crust. This crust has been observed as high as 2400 m. in the south of the region and 1800 m. in the north. Â
The lower snowpack is characterized by more crusts, the most notable is a rain crust from early November that is 50 to 130 cm deep. This crust is sitting near the base of the snowpack, surrounded by a weak layer of sugary facets. It is most likely to be reactive to human triggers in steep, shallow, rocky areas with a thin to thick snowpack.
Terrain and Travel
- Uncertainty is best managed through conservative terrain choices at this time.
- If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
- Be aware of the potential for large avalanches due to the presence of buried persistent weak layers.
- Remote triggering is a concern, watch out for adjacent and overhead slopes.
- Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
Problems
Persistent Slabs
A weak layer of surface hoar down 40-90 cm. has been reactive to human triggers, resulting in large avalanches.
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Wind Slabs
Lingering wind slabs may remain reactive to human triggers on a variety of aspects.
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Deep Persistent Slabs
A Crust buried near the bottom of the snowpack has been responsible for some very large explosive triggered avalanches up to size 4.
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Dec 28th, 2020 4:00PM
