Avalanche Forecast

Archived

Dec 7th, 2024–Dec 8th, 2024

Alpine

Natural avalanches possible, human triggered probable.

Treeline

Natural avalanches unlikely, human triggered possible.

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 unlikely, human triggered possible.

Treeline

Natural avalanches unlikely, human triggered possible.

Below Treeline

Natural avalanches unlikely.

Regions

Jasper, Brazeau, Churchill, Cirrus-Wilson, Fryatt, Icefields, Maligne, Marmot, Miette Lake, Pyramid.

Up to 25cm of new snow and strong winds have formed windslabs in leeward areas. Avalanches may have the potential to step down to deep persistent instabilities.

Confidence

Moderate

Avalanche Summary

Avalanche control on Saturday December 7th produced windslabs up to size 2 near Parkers ridge.

At Marmot Basin size 2 avalanches have been produced that are failing on the facets above the October 18 melt-freeze crust, over the past couple days . These have been produced by large explosives in the alpine.

Weather Summary

Sunday

A mix of sun and cloud with isolated flurries (trace). Alpine High -8 °C with mostly light ridge wind occasionally gusting to 45 km/h. Freezing level at valley bottom.

Monday

A mix of sun and cloud. Alpine Low -13 °C and High -10 °C. Ridge wind west (10 km/h). Freezing level at valley bottom.

Terrain and Travel Advice

Be mindful that deep instabilities are still present in the snowpack.
Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.

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.