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Avalanche Forecast

Archived

Feb 9th, 2023–Feb 10th, 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 unlikely, human triggered possible.
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 possible, human triggered probable.

Regions

Northwest Inland, Kispiox, Microwave-Sinclair, Ningunsaw, South Bulkley, South Bulkley, Telkwa.

Overnight flurries and steady south winds will continue to add to the storm slab problem. Stick to conservative terrain and give the new snow time to settle and bond.

Confidence

Low

Avalanche Summary

On Thursday, our field team observed 2 recent natural avalanches. With reduced visibility, the size 2 avalanches were 60-80 cm deep and suspected to have failed on a rain crust. A powder cloud was observed on Hudson Bay Mountain on Thursday morning as a natural avalanche occurred in one of the gullies.

On Wednesday, skiers triggered a large, size 2 avalanche near Ningunsaw. The Deep Persistent avalanche was triggered on an east aspect near ridgetop in a thin, rocky start zone and failed on basal facets.

Reports Tuesday documented a very large (size 3.5) natural deep persistent slab avalanche observed in the Babines on a northwest aspect around 1700 m and failing on basal facets 150 cm deep. This speaks to the importance of conservative terrain selection through this period of active weather. Several less surprising small to large (size 1-2.5) naturals were also observed in steep leeward terrain in the same area.

Observations from Monday in the snowier southwestern part of the region show our recent storm snow reacting to ski cutting, which produced numerous small (up to size 1.5) storm slabs on steep slopes at treeline and below with crowns up to 40 cm. Isolated natural releases were also observed in the alpine.

If you are out in the backcountry, please share your observations with the Mountain Information Network!

Snowpack Summary

15-30 cm snow accumulated in the region by end of Thursday, and strong south winds quickly promoted new slab formation over the day. Fresh snow adds to 50-80 cm of recent storm snow that has been getting continuously blown into wind slabs by southwest winds at treeline and above. The growing storm total sits on a crust from the warming event on January 25th and the bond at this interface is still in question, especially with forecast loading from new snow and wind.

The mid and lower snowpack continues to bond and stabilize. A few concerning weak layers can still be found in the top meter of the snowpack including a surface hoar layer from early January and a crust from late December.

Weather Summary

Thursday night

Flurries, 5-10 cm tapering overnight. South winds easing to 30 km/hr. Treeline low temperature -9 C with freezing level dropping to valley bottom.

Friday

Mostly cloudy with isolated flurries, 5 cm. Storm totals 15-30 cm. Southwest winds 20-30 km/hr. Treeline high temperature -5 C.

Saturday

Isolated flurries, up to 5 cm. Southwest wind gusting to 50 km/hr with approaching storm. Treeline high temperature -2 C.

Sunday

Snow, 10-20 cm. Southwest winds gusting over 60 km/hr. Treeline high temperature -2 C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Make observations and assess conditions continually as you travel.
  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent 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.

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.