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Avalanche Forecast

Archived

Dec 26th, 2013–Dec 27th, 2013

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

Regions

Little Yoho.

Wind and new snow will begin to push the Danger towards HIGH on steep loaded features. Stick to low angle terrain with low consequences. JBW

Weather Forecast

Another storm Friday will bring up to 10cm west of the divide with lesser amounts eastwards. Winds will continue to be in the Moderate to Strong range from the west. temperatures will cool with the passing of the front Friday/Saturday.

Snowpack Summary

Up to 10cm new snow has fallen west of the divide. Otherwise, the winds have been howling from the west and all windward slopes are stripped bare. Lee and cross loaded gullies have a mix of hard and soft wind slabs over a weak shallow base.

Avalanche Summary

No new avalanches have been observed over the last 24 hrs. Sporadic natural avalanches up to size 2.5 have been occurring this past week on steep slopes with wind loading.

Confidence

Wind effect is extremely variable

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.

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.