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Avalanche Forecast

Archived

Jan 23rd, 2023–Jan 24th, 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 unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

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

The snowpack remains sensitive to triggering. Expect as the strong winds and new snow continues, an already reactive wind slab will amplify in size.

Adopt terrain travel strategies that avoid steep areas on north-aspect terrain.

Confidence

Moderate

Avalanche Summary

Sunday: A remotely triggered avalanche was reported by skiers near the 4 lakes in the Babine mountains provincial park. This avalanche was a small (size 1.5) slab avalanche and was initiated while traveling from below. See the embedded MIN for pictures and details.

On Saturday both vehicle and skier remotely triggered avalanches have been reported. These avalanches were large (size 1.5 to size 2.5) and found on north aspect terrain between 1500 and 1600 m. A naturally occurring avalanche was reported as very large (size 3) in the same vicinity of the remote trigger avalanches.

Friday, poor visibility obscured observations. Avalanches were heard from steep terrain with powders clouds observed pluming out of lower runouts. Near Hazelton, one large (size 2) was observed, this naturally occurring avalanche was on a north aspect at 1600 m and was suspected to be initiated by a cornice collapse.

Strong southerly wind and light snowfall are expected to continue the formation of fresh wind slabs and build weak new cornice features. Avoid wind-loaded areas at upper elevations and keep in mind the potential for deeper instabilities to produce large and surprising avalanches.

Snowpack Summary

At upper elevations, southerly winds continue to scour windward areas and redistributed past and current storm snow into wind slabs in lee areas. Wind slab depth has been reported as up to 50 cm in depth and is likely to be much bigger given this information Is greater than 48 hours old.

Several persistent weak layers may be found in the top meter of the snowpack. Most prominently, a layer of surface hoar buried in early January is now 20-50 cm deep and is reactive to skier traffic. A weak layer of facets and/or surface hoar buried in late December is now down 70-110 cm.

In alpine terrain, triggering one of these layers is most likely on steep rocky slopes where they present as facets. In treeline terrain, the layers are most likely triggered on steep slopes in open trees where they present as preserved surface hoar.

In the north of the region, the lower-depth snowpack remains weak and heavily faceted.

Weather Summary

Monday night

Cloudy with light snowfall, 1 to 3 cm of accumulation. Alpine temperatures reach a high of -4 °C. Ridge wind southwest 60 km/h. Freezing level 500 m.

Tuesday

Cloudy with light snowfall, 1 to 3 cm of accumulation. Alpine temperatures reach a high of -2 °C. Ridge wind southwest 60 km/h gusting to 80 km/h. The freezing level will rise to 700 m.

Wednesday

Cloudy with light snowfall, 1 to 3 cm of accumulation. Alpine temperatures reach a high of 0 °C. Ridge wind west 60 km/h gusting to 100 km/h. The freezing level will rise to 1500 m.

Thursday

Cloudy with very light snowfall, and trace amounts of accumulation. Alpine temperatures reach a high of -2 °C. Ridge wind west 80 km/h. The freezing level will descend to 1000 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • Be aware of the potential for surprisingly large avalanches due to deeply buried weak layers.

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.

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.