A stable weather pattern to start the new year and possible temperature inversion mid-week. Consider the potential to trigger persistent slabs as the recent storm snow starts to finally settle and consolidate more rapidly.
Confidence
Moderate - Freezing levels are uncertain on Wednesday
Weather Forecast
MONDAY: Mix of sun and cloud / Light to moderate northwest wind / Alpine temperature -10 TUESDAY: Mix of sun and cloud / Light west wind / Alpine temperature -5, possible temperature inversion WEDNESDAY: Cloudy with sunny breaks / Light to moderate west wind / Alpine temperature -1, temperature inversion
Avalanche Summary
On Saturday a skier triggered size 2 persistent slab avalanche running on a layer of facetted snow from Mid December was reported. This happened in the north of the region's Dogtooth Range on a west aspect at 2400m. On Sunday there was also a report of a skier triggered avalanche near Mount Goldie just south of Invermere. There are no details on this avalanche at this time. Recent reports continue to show both natural and human triggered loose dry avalanches in steep terrain to size 1 and 1.5 in areas that have not been affected by wind. Additionally storm slab avalanches have been reported in the alpine to size 1.5. Expect continued potential for triggering loose dry avalanches in steep terrain and consider the potential to trigger persistent slabs where last week's storm snow has settled into a cohesive slab.
Snowpack Summary
20-40 cm low density new snow has accumulated and buried a recently formed layer of weak feathery surface hoar and/or sugary facets. Another layer buried mid-December that consists of surface hoar, sun crust and/or sugary facets is down approximately 40-70cm. The bond at this old snow interface is of critical importance where the overlying storm snow has consolidated into a slab. The most concerning areas are those that saw pronounced surface hoar development prior to mid-December, such as sheltered areas at and below treeline and any area where the surface hoar may have formed on top of a sun crust. Recent snowpack tests show wide ranging reactivity on this layer but suggest that it may be most reactive on northerly aspects. A rain crust that formed in late November is now buried 70-110cm deep. Recent reports show this layer to be unreactive at this time.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.