Avalanche Forecast
Regions: South Columbia.
Deeply buried weak layers continue to be a concern. If triggered, avalanches running on these weak layers will likely be large and destructive. Choose conservative terrain.
Confidence
Moderate - Uncertainty is due to how quickly the snowpack will recover and gain strength.
Weather Forecast
FRIDAY NIGHT: Cloudy with isolated flurries, light south wind, alpine temperature near -10 C.
SATURDAY: Scattered flurries, accumulation 5-10 cm, light to moderate southwest wind, alpine temperature near -8 C.
SUNDAY: Mainly cloudy with sunny breaks, light to moderate west wind, alpine temperature near -9 C.
MONDAY: Mix of sun and cloud, light west wind, alpine temperature near -10 C.
Avalanche Summary
On Wednesday there was a report of several size 3 to 4 explosives controlled deep persistent and persistent slab avalanches in the north of the region along the Highway 1 corridor. These ranged from south and east aspects to northeast running from the alpine to the valley floor.
Reports on Tuesday show a widespread storm slab and persistent slab avalanche cycle in the alpine and at treeline. Avalanches sizes ranged from size 1.5 to 3 on all aspects. Additionally reports from Tuesday in Rogers Pass indicate several natural and explosives controlled persistent slab avalanches to size 3.5-4 running full path from the alpine to the valley floor Monday night.Â
Snowpack Summary
60 to 100 cm of snow fell last weekend and on Monday night. Underneath this storm snow there is a sandwich of weak layers which are widespread throughout the region.
Just under the new snow, down about one meter below the surface is the mid December surface hoar. This layer had been failing naturally and has been quite sensitive to human triggering throughout the storm cycle. Large avalanches have been running on this interface connecting big terrain features.Â
Below that lies the early December persistent weak layer, it's about 80 to 140 cm below the surface. This weak layer is a mixed bag that often presents as surface hoar and facets sitting on top of a supportive crust. This is a nasty weak layer, when avalanches fail on it, they have been large and destructive. Smaller avalanches in motion can step down to this one too.
Terrain and Travel
- Be aware of the potential for large avalanches due to the presence of a persistent slab.
- If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
- Uncertainty is best managed through conservative terrain choices at this time.
Avalanche Problems
Wind Slabs
Wind switching directions has created wind slabs on a variety of aspectsÂ
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 2
Persistent Slabs
Recent storms have pushed the persistent slab problem over the tipping point resulting in very large avalanches. A slab rests on two persistent weak layer which has the capacity to propagate avalanches across terrain features.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Possible
Expected Size: 2 - 3.5