Avalanche Forecast

Archived

Dec 2nd, 2022–Dec 3rd, 2022

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.

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.

Early season conditions still exist in the Icefields Parkway. Ski with caution as the depth of snow is variable and shallow in many areas. Be on the lookout for wind slab in the Alpine and pay attention to signs of instability such as cracking and whumpfing as there is a persistent weak layer buried 25-30 cm below the surface.

Confidence

Moderate

Avalanche Summary

Sunday

Field teams observed no new avalanche activity in the last 48 hrs. Two old Loose Dry, Size 1 avalanches where noted in the Parkers Ridge area.

Snowpack Summary

In the Alpine, previous surface snow has been redistributed by winds from a variety of directions creating pockets of wind slab up to 20 cm thick near ridge top and on cross loaded features. There is a buried layer down 25-30cm that consists of Surface Hoar, Facets, and Sun Crust. Snow depth ranges from 40-100cm.

Weather Summary

A mix of sun and cloud.

Precipitation: Nil.

Alpine temperature: High -5 °C.

Ridge wind north: 10-25 km/h.

Freezing level: 1400 metres.

Monday

A mix of sun and cloud.

Precipitation: Nil.

Alpine temperature: Low -20 °C, High -14 °C.

Ridge wind northwest: 10-25 km/h.

Freezing level at valley bottom.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

Recent wind has varied in direction so watch for wind slabs on all aspects.
Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.