Regions
Kootenay Boundary.
Forecast strong winds, high freezing levels, and heavy rain or snow are expected to rapidly increase the likelihood of triggering slab avalanches.
Confidence
Moderate - Freezing levels are uncertain on Sunday
Weather Forecast
Cloud developing Saturday evening, and then strong southerly winds with 10-15 cm of new snow overnight. The freezing level is uncertain, some models (NAM and LAM) are showing close to 2500 metres overnight for specific points in the region, and the regional model is showing closer to 2000 metres. Another 15-20 cm of new snow (or rain) is expected during the day Sunday combined with strong southwest winds. Freezing levels dropping to 1000 metres by Monday morning. Mostly sunny on Monday with strong solar radiation and freezing levels around 1500 metres. Cloudy with light precipitation on Tuesday.
Avalanche Summary
Skier accidental, remotely triggered slab avalanches, and natural avalanches up to size 2.0 were reported on Friday. Explosives also released cornices up to size 3.0. On Thursday, a size 1.5 storm slab was ski cut on a northwest aspects at 2050m. This slab failed on the late-February surface hoar layer down 30-50cm. Numerous small ski cut avalanche were also reported to be failing on this layer through the region. Natural slab avalanche activity is expected during the storm on Sunday due to the combination of new snow or rain, strong winds, and warm temperatures, which is expected to overload the weak surface hoar layer from late February.
Snowpack Summary
Forecast rain and high freezing levels may rapidly increase the likelihood of triggering storm slabs and persistent weak layers. New snow and wind has added to the 30-50cm of recent storm snow that overlies a layer of well-developed surface hoar (up to size 20mm) which is very reactive to human triggers. This layer is widespread above 1700m except on south aspects where the interface was cooked by the sun and now exists as a buried sun crust. Significant wind transport has been noted so expect to find deeper, more destructive slabs in exposed lee terrain. 80-100cm below the surface you will likely find the mid-February crust/facet/surface hoar layer. Although this layer has become less likely to trigger, avalanches failing at this interface could be large and destructive.
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.