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Avalanche Forecast

Archived

Feb 27th, 2014–Feb 28th, 2014

Alpine
Natural avalanches possible, human triggered probable.
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 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

Kootenay Boundary.

We are entering a 'low probability/high consequence' phase with a tricky persistent weak layer. Check out this new blog post on difficult decision making and current conditions.Avoid large, unsupported slopes, especially on north aspects.

Confidence

Fair

Weather Forecast

Unsettled conditions are expected for Friday before arctic air moves into the region Friday evening. On Saturday and Sunday, weak disturbance from the south will mix with the cold air and may result in light scattered flurries.Friday: Mostly cloudy with sunny breaks, scattered flurries 2-8cm, treeline temperature around -8C, ridgetop winds 15-25 km/h variableSaturday: A mix of sun and cloud, scattered flurries 2-4cm, treeline temperature around -15C, ridgetop winds 10-20 km/h NE, outflow winds at valley bottomSunday: Mostly cloudy with sunny breaks, scattered flurries 2-4cm, treeline temperature around -12C, ridgetop winds 30-50 km/h SW

Avalanche Summary

Wednesday saw natural activity up to size 3 on SE through SW aspects triggered by solar warming.  Also reported were two skier remote triggered avalanches sized 1.5 and 2.  These were both triggered from 5m away and were 70cm deep.

Snowpack Summary

The primary concern is a ~1m thick slab from the last series of storms that is sitting on a stubborn persistent weak layer consisting of facets, surface hoar, melt-freeze crusts, or any combination of these. This weak layer is widespread at all elevations and aspects. Recent test results are suggesting that the layer is still easy to trigger in some areas but may becoming harder to trigger in other areas. We are still receiving isolated reports of large settlements or whumpfing which suggests the layer still has the potential for large propagations. In many areas the layer has the potential to produce large, destructive avalanches. The phase we are now entering is referred to a 'low probability/high consequence' problem. Continue to use conservative terrain choices until you are sure the layer is no longer unstable in your local area. Variable winds from the southwest through north have created touchy wind slabs on leeward slopes and cross-loaded features. In wind-loaded areas, slabs up to 2m thick may overlie the persistent weak layer.On south aspects, a sun crust has formed on the surface. New surface hoar formation 5-10mm has been observed.

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.

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.