Regions
Northwest Coastal.
There is some uncertainty as to how much snow is expected for Tuesday. Danger ratings will increase if amounts received exceed 5-15 cm as forecasted.
Confidence
Moderate - Intensity of incoming weather systems is uncertain on Tuesday
Weather Forecast
TUESDAY: Cloudy, flurries. Accumulation 5-15 cm. Ridge wind moderate, southwest. Temperature -2. Freezing level 600 m.WEDNESDAY: Snow. Accumulation 15-25 cm. Ridge wind light gusting to strong, west. Temperature +2. Freezing level 1700 m.THURSDAY: Mix of sun and cloud. Ridge wind light, northeast. Temperature -1. Freezing level 800 m.
Avalanche Summary
Sunday north of Meziadin Junction a natural size 4 and a natural size 3.5 were observed on a southwest and northeast aspect at 1800-2000 m and are suspected to have failed on the mid-January layer.On Saturday wind and storm slab avalanches failed naturally to size 2 on a variety of aspects in both alpine and treeline elevation bands. A natural size 3 persistent slab avalanche was observed on a steep north facing alpine feature with a crown up to 100 cm in depth, which suggests the mid-January interface was involved. A another very large avalanche (size 3.5) was reported from an unknown aspect/elevation. Natural avalanche activity was observed on Friday morning, producing several 30 cm thick slabs in the latest snow. A large (size 3) storm slab avalanche was reported on a east aspect east of Terrace.A few persistent slab avalanches released on Wednesday, most likely failing on the mid-January crust. This included a natural size 3 avalanche on a southwest slope at 1150 m near Exstew and a few skier triggered slabs (size 1-2) in thinner snowpack areas (east of Terrace and the northern part of the region).
Snowpack Summary
Another 15-25 cm of new snow since Sunday morning brings settled storm snow accumulations to 50-80 cm over the past week. A weak layer buried in mid-January is 100-140 cm below the surface and remains a concern. In most areas this layer is a crust, but it may also be surface hoar in sheltered areas at treeline and below. This layer produced a few human triggered avalanches throughout the region over the past week, and may remain reactive as it adjusts to the weight of the new snow.In thinner snowpack areas (north and inland), deeper crust / surface hoar layers that were buried in December and early January may still be a concern. They are buried over 150 cm below the surface, but may be triggerable from shallow spots.
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.