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Avalanche Forecast

Archived

Jan 27th, 2014–Jan 30th, 2014

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Waterton Lakes.

Wind slabs may develop Wednesday through Thursday with the 15-20 cm of new snow that is forecast. This could push the avalanche danger higher.

Weather Forecast

Dry and sunny on Tuesday with temperatures remaining below freezing for mid elevation. Westerly winds Tuesday night will create thin slabs on north and east lee terrain. Snow and light winds are forecast Wednesday through Thursday. Some reports say we may get 15-20cm.

Snowpack Summary

Cooler temperatures the past few nights have helped to strengthen the snowpack. Test results on Monday on NW and SE aspects did not show any significant concerns. Shallow snowpack areas still will have weak basal facet issues. The 6 - 10 cm of new snow that fell on Sunday morning helped to freshen up the previously wind or sun affected surfaces.

Avalanche Summary

TheĀ  6-10 cm of new snow from Sunday morning has resulted in minor sluffing from steep terrain on all aspects.

Confidence

Intensity of incoming weather systems is uncertain

Problems

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.