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Avalanche Forecast

Archived

Feb 4th, 2017–Feb 5th, 2017

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

Regions

Purcells.

Heavy snowfall is building touchy storm slabs in the mountains. Meanwhile, concern for persistent slab problems is increasing as the new snow adds load to the snowpack.

Confidence

Moderate -

Weather Forecast

Saturday night: Flurries bringing approximately 10 cm of new snow. Winds moderate to strong from the southwest.Sunday: Flurries delivering another 10-15 cm of new snow. Winds moderate to strong from the southwest. Alpine temperatures around -10.Monday: Flurries and periods of snow bringing 10-20cm of new snow. Winds light from the southeast. Alpine temperatures around -17.Tuesday: Cloudy with sunny periods and isolated flurries with a trace of new snow. Winds light from the west. Alpine temperatures of -15.

Avalanche Summary

Reports from Friday don't yet take our new snow into account, but loose snow sluffing in steep terrain (to Size 1.5) has been a developing theme in recent days, likely aided by faceting of surface snow. Reports from Thursday include details of explosives control in the north of the region producing results up to Size 1, with one cornice result succeeding in triggering a Size 2 slab over our December facet layer.On Monday, several natural wind slab avalanches up to size 2 were observed throughout the region. These avalanches occurred on most aspects and were mainly in the alpine. Since then, skiers and sledders have been triggering several wind slab avalanches up to size 1.5. A MIN report from the Quartz Creek area shows a sledder triggered size 2 wind slab avalanche. Click here for more details. As for Sunday's outlook, fresh storm slabs are expected to be sensitive to human triggering, especially where they overlie weak surfaces and in wind-exposed areas. With this in mind, the potential for storm slab avalanches to 'step down' to deeper weaknesses in shallow snowpack areas should not be overlooked.

Snowpack Summary

New snow over Friday and Saturday has now covered a range of different conditions that existed at our previous surface. In addition to wind slabs that exist on a variety of aspects in wind exposed terrain, the new snow will also overlie a sun crust reported on steep sun-exposed slopes as well as surface hoar recently found growing on sheltered open slopes. Surface faceting was also recently reported as a result of the current cold temperatures. The new snow's bond to these surfaces will likely be weak and touchy conditions can be expected as it settles into storm slabs above them. A persistent weakness buried mid January is now down 30-60 cm and consists of buried surface hoar in sheltered areas, sun crust on south aspects, and/or widespread faceted old snow. It has generally stabilized but may be sensitive to triggering in isolated areas where surface hoar is preserved. Another surface hoar/facet persistent weakness buried mid-December may be found down 600-110 cm, but is generally considered dormant. This and deeper persistent weaknesses remain an isolated concern in shallow snowpack areas where they lie closer to the snow surface.

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.