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Avalanche Forecast

Archived

Mar 17th, 2015–Mar 18th, 2015

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

Regions

Banff Yoho Kootenay.

Pockets of good skiing can be found in sheltered locations. Otherwise, ski conditions remain challenging.

Weather Forecast

Cloudy skies and minimal precipitation is forecasted for the next few days. Most of the precip will arrive Friday (~10mm equivalent). Temps at valley bottom will be hovering around zero degrees, cooler up high. Given the warmish temperatures and late time of year, any unexpected burst of solar energy will change conditions for the worse.

Snowpack Summary

Recent strong wind has created hard slabs on the snow surface in the alpine. Below this expect to find a mix of facets and crusts. As ghastly as that combination sounds, generally it is well bonded.

Avalanche Summary

A natural size avalanche size 1.5 was observed near the Balfour Hut today. The observer describes the avalanche as a hard windslab. It was noted at 2300m on a North aspect. No other avalanches were observed or reported.

Confidence

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.