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Avalanche Forecast

Archived

Jan 8th, 2018–Jan 9th, 2018

Alpine
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 possible, human triggered probable.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

Purcells.

The upper snowpack is starting to consolidate and have slab properties.  This snow sits above a buried weak layer at a depth prime to human triggering.  Cautious route finding is advised.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

TUESDAY: Cloudy with light snowfall, accumulation 5-15 cm, light to moderate westerly winds, alpine temperature near -8 C, freezing level near 1200 m.WEDNESDAY: Partly cloudy with intermittent flurries, light to moderate westerly winds, alpine temperature near -14 C, freezing level below valley bottom.THURSDAY: Cloudy with snowfall, accumulation 5-10 cm, moderate southwesterly winds, alpine temperature near -10 C, freezing level below valley bottom.

Avalanche Summary

A slab avalanche was noted in a lee feature in alpine terrain within the recent storm snow, about 15 cm deep.Numerous signs of instability have been noted in the snowpack over the past week, including whumpfing and cracking between 1700 and 2100 m, and two skier-triggered avalanches suspected to have released on the December 15 weak layer.  Expect the potential to trigger persistent slabs to increase as the snow continues to settle into a cohesive slab.Please share your recent observations through the Mountain Information Network.

Snowpack Summary

10-20 cm of new snow is forming a storm slab and sitting on surface hoar in sheltered slopes and a sun crust on steep solar aspects.  The snow fell with moderate to strong southwesterly winds in the alpine, which produced wind slabs in lee features at treeline and alpine elevations.  Below treeline, this new snow is mainly a concern in openings (e.g. cut blocks, gullies, cut banks).A warming trend and new snow is likely creating a dangerous slab above buried weak layers.  Dry snow overlies layers of weak and feathery surface hoar, with the deeper layer (December 15) buried 40 to 80 cm.  This layer is found most often around and below treeline but has been reported as high as 2450 m and could exist higher.  As the overlying dry snow becomes more cohesive and forms a slab, this layer has the potential to create easily-triggerable destructive slab avalanches.  This has occurred in neighbouring forecasting regions with a similar snowpack.Deeper in the snowpack (70 to 110 cm), a November crust is producing variable snowpack test results, from sudden fracture characters to no result.  This layer is considered dormant but could be triggered where the snowpack is thin.

Problems

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.

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.