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Avalanche Forecast

Archived

Dec 7th, 2012–Dec 8th, 2012

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

Regions

Northwest Coastal.

Confidence

Poor - Due to limited field observations for the entire period

Weather Forecast

Saturday: The effects of a weak ridge of high pressure will be brief. Generally broken skies with little to no precipitation for most of the day with a warm front pushing in for the late afternoon. Light to moderate amounts of snow are expected for the overnight period into Sunday.  Winds northwest 20 km/h for the daytime period changing to west 30-50km/h in the late afternoon. Alpine temperatures -8. Sunday: Moderate to heavy precipitation throughout the day with strong northwesterly winds. Alpine temperatures -3 degrees. Monday: Continued moderate precipitation with southwesterly winds 30km/h. Freezing levels expected at 800m with alpine temperatures -4 degrees.

Avalanche Summary

Explosives testing north of the Stewart region indicate avalanches running to size 2.5 in north facing terrain. These were isolated to the most recent storm snow. Any recent natural activity has been reported to size 1.5 and is also isolated to the recent storm snow.

Snowpack Summary

Up to 70 cm of new storm snow has fallen over the region in the past 5 days. This has been accompanied by strong winds from a wide variety of directions. Wind slabs continue to dominate the upper snowpack. Alpine and treeline surface snow conditions are variable with buried wind slabs, newly formed wind slabs and areas that are heavily scoured. Recent test results done in the upper storm snow show an easy resistant shear down 30-35 cm and a hard resistant down 80 cm. The mid-pack is gaining strength and is well settled.A November facet/crust layer can be found near the base of the snowpack. Tests done earlier in the week in the Bear Pass area around 1100 m have shown this layer to be unreactive. Testing done in the Shames area on this interface have also shown no results, with moist snow below. We do not have much recent information on this facet/crust interface, so it would be worth digging down yourself to test for its existence and reactivity.Total snowpack depth above 1000 m is 150-200 cm deep. Below 1000 m the snowpack shows a sharp transition from 100 cm dropping to 50 cm, and is generally below threshold.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.

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.