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 possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Regions
Cariboos.
There is a high degree of uncertainty regarding the weak layer that is below this past week's storm snow. Where this nasty layer exists, human triggering may be likely. Conservative terrain choices are key during times of high uncertainty.
Confidence
Low - Due to the number of field observations
Weather Forecast
Overnight WEDNESDAY: Cloudy with isolated flurries / Alpine Low -7 / Moderate, west wind / Freezing level 500 m.THURSDAY: Cloudy with isolated flurries / Alpine high -6 / Moderate, west wind / Freezing level 1000 m.FRIDAY: Cloudy / Alpine high -7 / Light to moderate, northwest wind / Freezing level 600 m.SATURDAY: Mix of sun and cloud / Alpine high -8 / Light, northeast wind / Freezing level 400 m.
Avalanche Summary
No avalanches were reported in this region on Tuesday. However, we currently have very few observations from within this region. Please post your observations to the Mountain Information Network. (MIN)
Snowpack Summary
Ongoing snowfall since Sunday night brings recent storm totals to 40-70 cm. This new snow sits on top of a weak layer of surface hoar (feathery crystals) and sun crust on steep south facing slopes. The surface hoar is most pronounced at treeline and below, but it may be found in sheltered alpine areas.At the base of the snowpack is a crust that formed in late October. There have been no reports of reactivity on this layer; however, this layer may be reactive to human triggers in isolated locations such as steep, rocky terrain, with a shallow snowpack. Small avalanches may step-down to this crust resulting in large, destructive avalanchesSnowpack depths decrease dramatically with elevation.
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.