New snow is adding to an already complex snowpack with a number of buried weak layers that have produced several recent, large avalanches. Moderate terrain with no overhead hazard is a good choice.
Avalanche Problem 1: Storm Slabs




- Avoid exposure to overhead avalanche terrain, avalanches may run long distances.
- If triggered, storm slabs may step down to deeper layers and result in large avalanches.
Avalanche Problem 2: Persistent Slabs




Several weak layers of concern are buried within the snowpack and have the potential to produce large avalanches. Conservative terrain with moderate-angled, supported slopes are good choices.
- Watch for signs of instability such as whumpfing, or shooting cracks.
- Be cautious in shallow snowpack areas where triggering a deeper weak layer is more likely.
Avalanche Summary
On Thursday and Wednesday, numerous natural, skier and explosive triggered storm slab avalanches up to Size 3 were reported with crowns from 20-80 cm deep, and propagations from 20 up to 150 m wide. These results were from predominantly north to east aspects between 1600-2000 m and ran long distances.
On Tuesday widespread sloughing and and several storm slabs up to Size 1 were observed in steep terrain. Also a Size 2 was triggered from 50 m away by a snow machine on a northeast aspect at 2050 m. The crown was 120 cm deep and is suspected to have failed on the mid-December weak layer.
Reports from Monday included seven deep persistent slabs that were released with small explosives in the alpine in the Fernie area. Sizes ranged from 2.5-3, crown depths averaged about 200 cm and all results indicated the deeply buried late-November crust as the failure plane. These results demonstrate the need for ongoing vigilance with regard to overhead hazards and the ongoing potential for deep, destructive avalanches to occur.
Snowpack Summary
About 60-80 cm of storm snow now covers a layer of surface hoar on sheltered aspects (especially prominent from 1400-1900 m) as well as sun crust on solar aspects that was buried mid-January.
Beneath the mid-January interface lie a number of very concerning buried weak layers. A layer of surface hoar from early-January is buried 90-110 cm below the surface. A weak layer buried mid-December (predominantly surface hoar and/or a sun crust) is around 120-160 cm below the surface at treeline and below treeline elevations. A rain crust with sugary facets that developed late-November is near the bottom of the snowpack. All of these layers have produced recent large, destructive avalanches and remain a concern.
Weather Forecast
TONIGHT: Light flurries. Accumulation 2-8 cm. Ridge moderate, west. Temperature -10. Freezing level lowering to valley bottom.
FRIDAY: Mix of sun and cloud, light flurries. Accumulation 2-8 cm. Ridge wind moderate, west. Temperature -5. Freezing level valley bottom.
SATURDAY: Cloudy, flurries. Accumulation 2-5 cm. Ridge wind light, southwest. Temperature -5. Freezing level valley bottom.
SUNDAY: Flurries. Accumulation 5-10 cm. Ridge wind moderate, southwest. Temperature -2. Freezing level 500 m.
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New snow and has formed touchy storm slabs and winds have loaded lee slopes near ridge top. These slabs have shown the potential for wide propagations and running long distances.