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Avalanche Forecast

Archived

Jan 12th, 2014–Jan 13th, 2014

Alpine
Natural and human triggered avalanches likely.
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

Purcells.

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Overnight : Flurries with trace amounts of precipitation, winds from the west at ridgetop 30 to 60 km/h, freezing level rising to 700m.Monday: Flurries with trace amounts of precipitation, strong winds from the W-NW at ridgetop gusting to 100 km/h, freezing level rising to 1200 M.Tuesday: No Precipitation in the forecast, moderate to strong winds from the west, freezing levels may rise to 1500m in parts of the forecast area.Wednesday: No Precipitation in the forecast, moderate winds from the west, freezing level should come down to 1200m in parts of the forecast area.

Avalanche Summary

There have been a number close calls with large avalanches in the north of this region in the last three weeks. Check out the incident database for more details. Recent reports of numerous skier controlled size 1 to 2's days indicate the severity of the new snow and wind loaded snow instability. There is a very real possibility that a small avalanche could "step down" to the weaker facetted layer at the base of the snowpack and produce a large destructive avalanche.

Snowpack Summary

Amounts of new snow are highly variable over the length of the forecast area, with the western parts of the range getting as much as 40 cm in the past 24 hrs, and the eastern and southern parts receiving 15 to 20. The new snow sits on a variety of snow surfaces including older wind slabs and a soft layer of facetted snow and/or surface hoar. These sit on top of older wind slabs and a couple of persistent weak layers that exist in the upper meter of the relatively thin snowpack. The mid December surface hoar is buried around 30-90 cm. The early December facet/crust combo is buried down 50-150 cm. Both interfaces give variable results with snowpack tests, but professional operators are treating them with caution.A big concern, especially in the northern part of the region is a layer of weak sugary depth hoar crystals at the base of the snowpack that lie above a crust from early October. Several large avalanches in the last two weeks have been attributed to failures at this layer. Wide propagations on relatively gentle terrain have been noted, as well as a tendency for seemingly disconnected slopes to propagate over a wide area and produce large avalanches.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.