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Avalanche Forecast

Archived

Nov 28th, 2014–Nov 29th, 2014

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

Regions

South Rockies.

A Special Public Avalanche Warning is in effect. An intense burst of snow is forecast overnight Friday which may cause a spike in avalanche danger.

Confidence

Poor - Forecast snowfall amounts are uncertain

Weather Forecast

Very cold arctic air is heading southwards. At the boundary between this cold air and the current warm, moist air, an intense burst of snowfall snowfall is anticipated. Friday night: 20-40 mm precipitation, falling as snow (this could make deep dry snow). Temperatures plummeting. Strong SW winds easing by morning.Saturday: Light snow may continue through the day. Becoming cold and clear by the end of the day. Light winds.Sunday/Monday: Very cold and dry. Light winds.

Avalanche Summary

Explosives triggered two very large (size 2.5 and 3.5) slabs in the south of the region on Thursday around treeline. These failed on a weak layer of facets buried about a week ago. In the north of the region, numerous shallow size 1.5 slabs failed below treeline. Over in the neighboring Lizard/Flathead region, natural and human-triggered avalanches to size 2 have been reported this week. These either failed on basal facets or at the interface below the recent storm snow.

Snowpack Summary

As we begin our forecasting season, we are working with very limited field data. If you have been out in the mountains, we'd love to hear from you. Please email us at [email protected] weather over the past month has created a snowpack full of problems! A weak layer (of facets over a crust) which formed during November's dry spell is now buried a metre or so down. Now it is overloaded with wind-deposited or just plain deep storm snow and we have started to see some very large avalanches in the south of the region. In the upper snowpack, changes in wind and temperature have led to storm slab development. In rain-soaked zones below treeline, the snowpack has been very weak while wet, but should lock up once the deep freeze hits. Add an incoming burst of heavy snow to low levels, and we are likely to see natural avalanches spilling down steep headwalls, with the chance of triggering one of these deeper weaknesses to create a very large avalanche. A good weekend to be cautious while the snowpack has a chance to settle down.

Problems

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.