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Avalanche Forecast

Archived

Dec 2nd, 2013–Dec 3rd, 2013

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 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

Glacier.

Our next persistent weak layer is now buried down 30-40cm. Be careful in your route selection to minimize exposure.

Weather Forecast

Lingering flurries today with temperatures cooling off. Winds are expected to pick up from the north gusting to 65km/h. Skies clearing tomorrow and into the week with temperatures plummeting from an arctic high pressure ridge pushing into the province.

Snowpack Summary

30-40 cm of recent storm snow sits over the November 28 surface hoar/crust layer which had widespread distribution. The November 12 surface hoar layer present at higher elevations is down 60-120cm

Avalanche Summary

6 natural slab avalanches size 2.0 were observed east of the Rogers Pass summit from Mt Macdonald and Mt Tupper yesterday.

Confidence

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.