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Avalanche Forecast

Archived

Apr 12th, 2014–Apr 13th, 2014

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

Regions

Little Yoho.

Spring conditions are here. Excellent skiing on high North aspects and supportive travel early in the day! The hazard will rise as the temperatures heat up during the day. Start your trips early and be off of big slopes before they heat up. CJ

Weather Forecast

Sunday looks like a cool clear day with overnight lows around -12`C, light W winds and freezing levels near 1700m.  Monday will see increasing cloud, Light SW winds, alpine temperatures up to -2 and freezing levels near 2000m. Tuesday will see some snow flurries, freezing levels near 2000m and light W winds.

Snowpack Summary

10-12cm of new snow over a supportive crust on all aspects and elevations today. Some moist snow at lower elevations. Snow pack becoming isothermal below 1700m later in the day. Small wind slabs present near ridge crests in the alpine from strong NW winds.

Avalanche Summary

Some loose sluffing out of steep terrain today up to size 1. In the past several days we saw numerous slab avalanches on all aspects and elevations up to size 3 failing on basal facets when the temperatures got really warm. Loose wet avalanches and cornice failures were also observed.

Confidence

Freezing levels are uncertain on Tuesday

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.