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Avalanche Forecast

Archived

Feb 28th, 2018–Mar 1st, 2018

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
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 possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Northwest Coastal.

Storm snow and wind continue to overload the snowpack. Strong outflow winds and light snowfall are expected to continue into Thursday. Choose conservative terrain and avoid overhead hazard. Recent large avalanches have run long distances.

Confidence

Moderate - Wind effect is extremely variable

Weather Forecast

TONIGHT: Flurries. Accumulation 5-10 cm. Ridge wind strong, east. Temperature near -6. Freezing level 500 m.THURSDAY: Cloudy, flurries. Accumulation up to 5 cm. Ridge wind moderate to strong, east. Temperature near -5. Freezing level 300 m.FRIDAY: Mix of sun and cloud. Ridge wind moderate, east. Temperature near -5. Freezing level valley bottom.SATURDAY: Sunny. Ridge wind light, east. Temperature near -10. Freezing level valley bottom.

Avalanche Summary

On Wednesday and Tuesday we received a reports of two very large (size 4 and 4.5) natural avalanches that are suspected to have failed on a deep weak layer near the base of the snowpack. The larger of these occurred near Snowbound Creek west of Terrace on a south aspect at 1400 m and ran full path from ridge top to valley bottom, destroying a significant amount of mature forest beyond it's historical trimlines. Skier controlled and natural wind slab avalanches up to size 2 were also reported on Tuesday on north to east aspects between 1200-1400 m.Evidence of a widespread natural cycle up to size 3 was reported from Sunday and Monday. And explosive control work on Monday produced numerous size 2.5 - 3 storm slabs on southeast through southwest aspects at all elevations.Skiers in the Shames area on Sunday reported reactive storm slabs up to size 2 on south and west aspects. Read the MIN report here.In the north (colder & drier inland area) near Ningunsaw there was a remotely triggered size 2.5 avalanche on Sunday with a hard slab releasing near the ground in shallow snowpack area with a gentle start zone.

Snowpack Summary

Recent storm snow accumulations of 50-100 cm have been affected by ongoing moderate to strong westerly winds at alpine and treeline elevations. Recent storms are burying older hard wind slabs and scoured surfaces in wind-exposed areas. In wind-sheltered terrain, sun crusts or dry facets sit below the recent storm snow.In the upper pack about 100-150 cm deep, is an interface of sun crusts, facets and spotty surface hoar (which is most prevalent in sheltered treed locations) that was buried mid-February. Deeper in the snowpack, around 150-200 cm down, you'll find a crust/surface hoar layer from January which still has the chance to surprise you and could be triggered from a thin snowpack spot, or with a large trigger like cornice fall. Basal facets may be found near the bottom of the snowpack in colder / drier parts of the region.

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.