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Avalanche Forecast

Archived

Jan 4th, 2014–Jan 5th, 2014

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

Regions

Northwest Coastal.

Confidence

Fair - Freezing levels are uncertain

Weather Forecast

Sunday: Partly cloudy with sunny breaks. Warm air in the alpine, above freezing to about 2000 metres. Strong Southwest winds.Monday: Strong Southwest winds becoming moderate Westerly. Warm air is expected to remain in the alpine with freezing levels around 1700 metres.Tuesday: Mostly cloudy with light Southwest winds and seasonal alpine temperatures.

Avalanche Summary

Explosive control in the Ningunsaw area released from size 1.5 dry slab up to one size 3.5 that released or stepped down to the ground. Natural avalanches up to size 2.5 that ran during the storm were reported from flights through remote areas.

Snowpack Summary

In general the snowpack seems shallower and more faceted in the northern part of the region, and deeper with more wind and storm slab problems in the south. A significant amount of recent storm snow is settling rapidly, but will likely remain unstable for at least a few days after the weather clears. However, persistent weaknesses including facets and surface hoar buried near the end of December, will likely remain primed for triggering. Basal facets remain a concern in shallow snowpack areas and an overlying snowpack structure favoring step-down fractures can contribute to the persistence of this deep slab problem.

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.

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.