The danger has come down, but large human triggered avalanches remain possible. Start with small test slopes and build up slowly to the bigger terrain features. There is still a lot of uncertainty associated with this early winter snowpack.
Weather Forecast
A northwest flow will bring light snowfall, and cool temps throughout the forecast period. TUESDAY: Flurries bring up to 2cm of snow, light northwest winds, -5 at 1500m. WEDNESDAY: More flurries for the central Purcells, northwest winds, THURSDAY: Overcast, light northwest winds.
Avalanche Summary
Avalanche activity appears to have tapered off since Friday. Reports from over the weekend describe mainly small explosively controlled avalanches in steep terrain. The exception was a small skier triggered avalanche that ran on the December 2nd surface hoar near in the Panorama slack country. On Friday two significant observations were reported: The first was a natural size 3.5 avalanche that was observed on a SE facing feature at 2800m in the Bugaboos. It ran to ground in some places. The second was a report of a skier triggered size 2.5 avalanche in the DogTooth range that was accidentally triggered on an east facing feature at 1500m. This avalanche failed on the early December Persistent Weak Layer.
Snowpack Summary
Between 35 to 80cm of snow fell last week in the Purcells. You may find a thin crust about 10 to 30cm below the snow surface as high as 1800m. Below the new snow lies the early December persistent weak layer. This layer may be found as either an old sun crust on south facing features in the alpine, or as large grained surface hoar and small facets in isolated pockets especially between 1400m and 1800m. Recent test results on this interface have been widely variable. "Resistant planar," "sudden collapse" and even "no result" have been reported from test profiles as recently as Dec. 13th. All the variation in trigger sensitivity makes this layer tricky to manage. The mid and lower portions of the snowpack are thought to be well settled although a basal weakness may be lurking on high elevation alpine features.
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.