Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Regions
Cariboos.
It will take a few days for the most recent storm snow to settle and bond. A cautious approach is recommended.
Confidence
Moderate - Forecast snowfall amounts are uncertain
Weather Forecast
THURSDAY: Cloudy with isolated flurries, accumulation 5-15cm, light to moderate southwest winds, Alpine temperature -2FRIDAY: Cloudy with isolated flurries, light southwest wind, alpine temperature -2SATURDAY: Mix of sun and cloud, wind light southeast, alpine temperature -8More details can be found on the Mountain Weather Forecast.
Avalanche Summary
Recent reports indicate a size 2.5 remotely triggered avalanche 70cm deep and running on a west aspect at 2100m.
Snowpack Summary
The most recent storm brought variable snow fall amounts to this region. The storm slab is expected to be sensitive to light additional loads, and may release naturally with continued loading from new snow and wind. Previous to the new storm, recent cold and clear weather has promoted both faceting of surface snow as well as the growth of surface hoar that has been reported to be up to 7mm in size in sheltered areas below treeline. Below the surface, our recent storm snow was redistributed by moderate to strong southwest and more recent northerly winds in exposed upper areas. In deeper snowpack parts of the region, the mid-December facet layer lies up to 120 cm below the surface. In these areas, professionals feel this layer has generally gained considerable strength. In shallower areas, particularly those in the southeast (Allen Creek), North (Sugarbowl) and likely some western areas around Quesnel and Barkerville, the snowpack is likely a lot more suspect, with a thicker, more pronounced facet layer buried only 50-60 cm below the surface.
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.