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Avalanche Forecast

Archived

Feb 4th, 2023–Feb 5th, 2023

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

Regions

North Columbia, South Columbia, Esplanade, Jordan, North Selkirk, Shuswap, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, North Okanagan, Retallack, Valhalla, Whatshan.

Reactive storm slabs may be evident underfoot, particularly in wind-loaded areas, but keep the potential for large, destructive deep persistent avalanches in the forefront of your mind.

Confidence

Moderate

Avalanche Summary

On Friday, numerous natural wind slabs were observed in the alpine and treeline up to size 2.5. One very large (size 4) deep persistent slab was observed on a south aspect in the alpine.

On Thursday, numerous natural and human-triggered storm and wind slabs were observed throughout the region up to size 2.5. One natural persistent slab avalanche (size 2.5) was observed in the Valhalla mountains. It initiated as a wind slab, stepped down to mid-snowpack weak layers, and then gouged to the basal facets, stepping down to the ground.

Last weekend, various deep persistent slab avalanches were also triggered naturally, being large to very large (size 2 to 4). The avalanches occurred on all aspects between 2400 and 2800 m.

High-consequence avalanche activity is ongoing for several weeks now. Most of the avalanches over the past week were released between 1800 and 2800 m, on all aspects.

Your best defence is to stay diligent in choosing low-consequence terrain away from overhead exposure.

See more on the potential of triggering deeper weak layers in Forecasters' Blog.

Snowpack Summary

Stormy weather over the past week has brought 30 to 80 cm of new snow to the region. Snowfall will continue throughout the day bringing an additional 5-15 cm. Warm windy weather is causing this storm to settle into reactive slabs, especially on leeward slopes that may see more loading from the wind. This storm snow sits above a plethora of old snow surfaces including previously wind-affected snow at upper elevations, a sun crust on steep solar aspects, faceted snow, and surface hoar crystals in wind-sheltered terrain.

Below the recent snow is a crust that extends up to 1800 m in the northern part of the region and up to 2000 m further south. This crust is buried about 40 to 100 cm deep and may host small facets on the crust.

Deeper in the snowpack two layers of surface hoar which formed in early January are 60 to 120 cm deep. These weak layers are still on our radar, although snowpack tests are indicating they may be strengthening.

Large and weak facets from November are near the base of the snowpack, which continue to produce very large avalanches in the region, as described in the Avalanche Summary.

Weather Summary

Saturday night

Cloudy with clear periods and isolated flurries, up to 5 cm accumulation. Alpine temperatures drop to a low of -5 °C. Mostly light ridge wind occasionally gusting to 40 km/h from the southwest. Freezing level drops to 500-1000 metres.

Sunday

Cloudy with snowfall, 5-10 cm accumulation. Alpine temperatures reach a high of -2 °C. Mostly light ridge wind occasionally gusting to 45 km/h from the southwest. Freezing level 1300 metres.

Monday

Cloudy with snowfall, 2-10 cm accumulation Alpine temperatures reach a high of -3 °C. Ridge wind 25 to 55 km/h from the southwest. Freezing level 1400 metres.

Tuesday

Cloudy with snowfall, 5-10 cm accumulation. Alpine temperatures reach a high of -1 °C. Ridge wind southwest 30 to 50 km/h. Freezing level 1600 metres.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Storm snow and wind is forming touchy slabs. Use caution in lee areas in the alpine and treeline.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Be mindful that deep instabilities are still present and have produced recent large avalanches.
  • Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.

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.

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.