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Avalanche Forecast

Archived

Dec 12th, 2017–Dec 13th, 2017

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

High freezing levels continue but precipitation amounts overnight Tuesday vary through the region. If you receive more than 20 mm consider the avalanche danger to be CONSIDERABLE.

Confidence

Moderate - Forecast snowfall amounts are uncertain

Weather Forecast

Wednesday: Mostly cloudy with sunny breaks. Alpine temperatures near plus 5 degrees and freezing levels up to 3000 m. Ridgetop winds moderate from the south.Thursday: Moderate precipitation amounts. Alpine temperatures high of plus 6 degrees with freezing levels 2500 m. Ridgetop winds strong from the southwest. Friday: Cloudy with some flurries. Alpine temperatures near -3 and freezing levels dropping to 800 m. Ridgetop winds light gusting strong from the southwest.Check out the Mountain Weather Forecast for more detail.

Avalanche Summary

On Monday, numerous natural wet slab avalanches up to size 2.5 were reported from upper elevations. Avalanche activity will likely increase through the forecast period with new rain, snow and wind.I'd also remain suspect of the deep persistent layers on your radar as the region receives this new load. On December 7th and 8th a few deep persistent slabs to size 3 out of steep south facing alpine terrain in the Skeena corridor west of Terrace were reported. Basal facets were thought to be the culprit in these events. The deep persistent slab is something to keep on your radar, especially with more weather in the forecast.

Snowpack Summary

Recently, the region has received up to 20 mm of rain and some new snow at high alpine elevations. The alpine and treeline has seen significant wind effect on all aspects including wind slab and wind pressed snow. Snow surfaces are highly variable and consist of rain crusts, moist snow and new dry storm snow at elevations above 1700 m. Below the surface sits a well-settled snowpack overlying several layers of interest. Down 70-100 cm you'll likely find a 5-10 cm thick crust which was buried on November 23 and in some areas, a feathery surface hoar layer down 50-60 cm producing moderate snowpack test results. The widespread crust/facet interface that was buried at the end of October can now be found 100-200 cm deep and exists region wide.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.

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.