Avalanche Forecast

Archived

Jan 23rd, 2025–Jan 24th, 2025

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.

Below Treeline

Natural avalanches unlikely.

Regions

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

Better skiing might be found around tree line after a few days of wind, affecting a variety of aspects and elevations.

Be mindful of wind slabs in unexpected places.

Confidence

Moderate

Avalanche Summary

No new avalanches observed during road patrol from Jasper to Saskatchewan Crossing January 22nd.

A couple of wind slabs up to size two were observed on Sunwapta Peak and Nigel Peak on the 19th.

Avalanche control near Parkers on Friday Jan 17th produced slab avalanches up to size 2.5. These avalanches stepped down to the Deep Persistent layer.

Snowpack Summary

Widespread wind effect in the TL and Alpine regions. Wind slabs sit on a very weak faceted mid pack. At the bottom of the snowpack are the early season crusts, which are often surrounded by large depth hoar. The snowpack is 70-130 cm in depth at treeline. Valley bottom travel is difficult in the weak, loose facets.

Weather Summary

FridaySunny with cloudy periods.

Precipitation: Nil.

Alpine temperature: High -12 °C.

Ridge wind northwest: 15 km/h gusting to 40 km/h.

Saturday

Sunny with cloudy periods.

Precipitation: Nil.

Alpine temperature: Low -12 °C, High -5 °C.

Ridge wind northwest: 10-20 km/h.

Sunday

Sunny with cloudy periods.

Precipitation: Nil.

Alpine temperature: Low -5 °C, High 1 °C.

Ridge wind northwest: 10 km/h.

Terrain and Travel Advice

Be careful with wind-loaded pockets, especially near ridge crests and rollovers.
Avoid exposure to overhead avalanche terrain; avalanches may run surprisingly far.

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.