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Avalanche Forecast

Archived

Dec 22nd, 2019–Dec 23rd, 2019

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

Little Yoho.

Avalanche control of Mt Bourgeau Monday December 23. Please avoid activity anywhere on Mt Bourgeau and Eagle slide paths.

Enter terrain very cautiously and avoid exposure to overhead hazard. Avalanche conditions will take some time to improve.

Weather Forecast

Overcast skies and light flurries are forecasted for Monday with little to no snow accumulation. Temperatures on Monday will reach a high of -5 in the valley before a gradual cooling trend sets in for the remainder of the week. Expect wind values to stay in the light to moderate range.

Snowpack Summary

30-60cm of settled storm snow since Friday has formed storm slabs all elevations and aspects. At upper elevations evidence new wind transport is visible. Below the new snow the snowpack structure is generally weak, consisting of facets and depth hoar and a Nov crust up to 2500m. These weak layers are getting overloaded with all of the new snow.

Avalanche Summary

Good visibility today revealed widespread natural avalanche activity to size 3 on all aspects and elevations from the past 48 hours. A noteworthy observations was the effect of the warm temps and rain at lower elevations causing widespread storm slab releases below tree line. Avalanche control today produce numerus slab releases to size 3.

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.

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.

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.