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Avalanche Forecast

Archived

Feb 5th, 2015–Feb 6th, 2015

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
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 possible, human triggered probable.

Regions

Northwest Coastal.

Extreme wind and heavy snowfall should ramp up Thursday evening. Only the most conservative non-avalanche terrain is appropriate this weekend.

Confidence

Fair

Weather Forecast

Extreme southerly winds in the alpine along with strong east through south winds below treeline are expected through the forecast period. The freezing level should stay right around 600m and a few significant shots of precipitation are expected. 10 to 40 cm are possible Thursday night, another 10 to 40cm are expected Friday with 5 to 25cm on tap for Friday night. Fore a more detailed look at this dynamic weather pattern visit avalanche.ca/weather

Avalanche Summary

On Wednesday, (before the storm) a size 2.5 wind slab avalanche was reported from a steep SE facing feature at 1300m. I suspect there will be more activity to report on in the next few days.

Snowpack Summary

35- 60cm of new snow has fallen in the last few days. Strong winds have redistributed this snow in exposed terrain forming winds slabs in leeward features and stripping exposed slopes. The late-January crust is typically down 100-140cm in the south of the region and about half this depth in the north. Tests are indicating that this interface is generally well bonded but isolated avalanches have been reported to have released on this layer recently. The mid-January rain crust and/or surface hoar layer is down over 150cm in the south and has generally become inactive. It may still be a concern in thinner snowpack areas. The November crust/facet combo near the bottom of the snowpack is thought to be generally well bonded. However, this deep and destructive layer is still reported to be reactive in the far north of the region.

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.