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.
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
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
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.