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Avalanche Forecast

Archived

Feb 8th, 2017–Feb 9th, 2017

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, human triggered possible.

Regions

Northwest Coastal.

Use extra caution as you transition into wind affected terrain

Confidence

Moderate - Forecast snowfall amounts are uncertain on Friday

Weather Forecast

THURSDAY: Cloudy with sunny periods / Light northeast wind / Alpine temperature -10 FRIDAY: Cloudy with flurries, accumulation 5-10cm / Moderate to strong southwest wind / Alpine temperature -5SATURDAY: Snow, accumulation 20-30cm / Moderate to strong southwest wind / Alpine temperature -1More details can be found on the Mountain Weather Forecast.

Avalanche Summary

No new avalanches were reported in the past few days. The most recent avalanche activity was reported on the weekend. This activity included skier triggered wind slab activity to size 1, explosive triggered wind slab avalanches to 2.5 and 3. Some of these avalanches in the Bear Pass area released on weaknesses near the base of the snowpack. In the northern most parts of the region near Bell2 or Ningunsaw, there are still reports as recent as Saturday of natural and skier triggered avalanches to Size 2.5 stepping down to basal facets in the alpine and at treeline.On Thursday, expect recently formed wind slabs to remain reactive to human triggering. Outflow winds have continued to add additional load to these wind slabs in places where there is still snow available to be redistributed. A basal weakness continues to drive a low probability/high consequence problem for shallow snowpack areas, especially in the north of the region.

Snowpack Summary

Widespread wind affected surfaces are being reported in exposed terrain including scoured surfaces, sastrugi, and hard wind slabs. In areas sheltered from the wind, the surface snow is reported to be faceting and surface hoar is developing. Below around 1100 m elevation, a rain crust can be found near the surface of the snowpack. Deeper in the snowpack, the mid-January surface hoar/facet layer is now typically down 70-100 cm. Recent observations suggest the layer has generally stabilized but isolated weaknesses may still exist, especially where buried surface hoar is still intact. Below this layer, the snowpack is generally strong and well settled. The exceptions are areas around Bear Pass and Ningunsaw where basal facets remain an ongoing concern, especially in shallow snowpack areas.

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.