Recent storm totals vary across the region. Pay close attention to how much snow fell in your area as this will affect your localized hazard. For more details, check our latest Blog Post: http://www.avalanche.ca/blogs/VLsBsCgAACYAJdfM/mid-jan-sh
Confidence
Fair - Due to the number of field observations
Weather Forecast
Expect generally cloudy skies with occasional sunny breaks on Tuesday and Wednesday as a dry weak ridge develops over the southern half of the province. By Thursday it looks like the ridge may break-down somewhat allowing for moist pacific system to enter the region from the northwest. If this happens, accumulations will likely be light. Winds should remain light to moderate from the west-northwest. Freezing levels will hover around 800m on Tuesday and Wednesday, and then rise to about 1000m on Thursday.
Avalanche Summary
No avalanche activity was reported in recent days. I'm very confident that was due to a lack of observations rather than actual conditions. In deeper snowpack areas I'm sure there was a decent round of storm slab activity failing on the recently buried surface hoar. Due to the persistent nature of these crystals, I expect continued human triggered storm slab avalanche activity in these areas. Avalanche activity is generally unlikely on deeper persistent weaknesses. That said, a surface avalanche in motion could "step down" to a deeper, more destructive layer.
Snowpack Summary
Between 15cm and 40cm of recent snowfall has buried widespread 10-20mm surface hoar and a sun crust on steep sun exposed slopes. Strong winds have blown these accumulations into deeper deposits in higher elevation terrain. Due to the underlying surface hoar, I would expect continued touchy conditions, especially in areas where the recent snowfall exists as a cohesive slab.The mid-December surface hoar/crust layer is typically down 60-120cm below the surface. The reactivity of this persistent weak layer appears to be quite variable but still has the potential for large, destructive avalanches in some areas. The layer appears to be the most reactive at and below treeline. The mid-Nov weak layer is near the bottom of the snowpack but has generally become inactive.
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.