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Avalanche Forecast

Archived

Apr 7th, 2018–Apr 8th, 2018

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 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

South Rockies.

New snow, strong winds and rising freezing levels are increasing avalanche danger for the forecast period. Choose conservative terrain and be especially wary of overhead hazards as the day warms or the sun shines.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

TONIGHT: Cloudy, flurries. Accumulation 10-15 cm. Ridge wind strong, west. Alpine temperature near -7. Freezing level 500 m.SUNDAY: Cloudy, flurries. Accumulation 2-6 cm. Ridge wind moderate to strong, west. Alpine temperature near -3. Freezing level 1800 m.MONDAY: Mostly sunny. Ridge wind moderate, west. Alpine temperature near 0. Freezing level 2100 m.TUESDAY: Increasing cloud. Ridge wind moderate to strong, southwest. Alpine temperature near +4. Freezing level 2600 m.

Avalanche Summary

On Friday both natural and easily skier-triggered wind slab releases up to size 1.5 were reported in the southern part of the region, while several loose dry avalanches were reported in the Crowsnest Pass area. Read recent MIN report here. Thursday in the Elkford area, recent small (size 1) loose/dry avalanches were reported on northerly aspects while loose/wet were observed on solar aspects. In the southeast corner of the region skier-triggered loose/dry avalanches were reported to be running far on a recently buried crust.Wednesday small loose wet point releases were reported from steep rocky solar aspects.On Tuesday, small avalanches were observed in the Alexander Creek area. On Monday, small natural avalanches were reported from the region, and ski cutting produced similar small avalanches on wind-loaded features. Also on Monday, explosives triggered one size 2 wind slab avalanche on an east aspect at 2300 m. This avalanche ran on a 60 cm deep crust layer.

Snowpack Summary

10-15 cm of snow sits above a variety of crusts on all but high north aspects. Northern parts of the region have less new snow than southern parts. Wind has formed hard slabs in lee features, and in some cases the snow may be poorly bonded to the crusts.Multiple crusts exist in the top metre of the snowpack. Some parts of the region may have a surface hoar layer roughly 60 cm deep on north aspects at treeline.A well settled midpack sits above sugary facets in many parts of the region, especially thin snowpack areas.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.