Avalanche Forecast

Archived

Feb 27th, 2024–Feb 28th, 2024

Alpine

Natural and human triggered avalanches likely.

Treeline

Natural and human triggered avalanches likely.

Below Treeline

Natural avalanches possible, human triggered probable.

Alpine

Natural and human triggered avalanches likely.

Treeline

Natural and human triggered avalanches likely.

Below Treeline

Natural and human triggered avalanches likely.

Alpine

Natural and human triggered avalanches likely.

Treeline

Natural and human triggered avalanches likely.

Below Treeline

Natural avalanches possible, human triggered probable.

Regions

Banff Yoho Kootenay, Little Yoho, Banff, East Side 93N, Kootenay, Lake Louise, LLSA, Sunshine, West Side 93N, Field.

The biggest storms of the season are upon us along with touchy avalanche conditions. Now is a good time to stay out of avalanche terrain and enjoy the new snow in simple terrain or at your local ski hill!

Confidence

High

Avalanche Summary

Forecasters have observed continued evidence of a widespread avalanche cycle following the recent storm.

Avalanche control on Mt Whymper (Kootenay NP) on Tuesday produced size 2-3 avalanches with every shot. The crowns were 40-100 cm deep and the failure planes were the recent storm snow sliding on the Feb. 3rd crust and occasionally stepping down to ground.

Snowpack Summary

30-60 cm of recent snow sits on top of the Feb 3rd crust/ facet layer. This crust is variable in thickness and exists up to 2500m (higher on solar aspects). In thinner eastern areas, the mid and lower snowpack are weak and facetted.

Average snowpack depths at treeline range from 80 cm in thinner eastern areas to 150 cm in thicker western areas.

Weather Summary

A low pressure system is arriving overnight Tuesday that will bring 30-50 cm of snow warmer temperatures and strong SW winds.

Wednesday: 5-10 cm, strong SW winds, ~ 1800m freezing levels

Thursday: 15-30 cm, strong SW winds decreasing to moderate in the afternoon. Freezing levels dropping to valley bottom

Friday: System clears, potential for upslope snow.

Click here for a more detailed weather forecast

Terrain and Travel Advice

Avoid all avalanche terrain during periods of heavy snowfall.
Avoid exposure to overhead avalanche terrain, large avalanches may reach the end of run out zones.
Storm slabs in motion may step down to deeper layers resulting in large avalanches.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.