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Avalanche Forecast

Archived

Jan 21st, 2023–Jan 22nd, 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 light 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 that will certainly harbor new and existing reactive wind slabs.

Confidence

Moderate

Avalanche Summary

Friday, poor visibility obscured observations. Audibles were heard from steep terrain and powders clouds were observed pluming out of lower runouts. Near Hazelton, one 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.

On Thursday, low visibility impeded visual observations., however, numerous audible avalanches have been reported. Additionally, observation of powder clouds pluming out of very steep extreme terrain was reported.

On Wednesday, professional operations reported a natural windslab avalanche cycle of large avalanches (size 3). These avalanches initiated in the alpine, on steep north aspect terrain near ridgetop. Moderate to strong southwest wind loading was the suspected trigger. Due to the size of these avalanches, it is suspected that they had stepped down to the lower/mid-pack PWLs.

The incoming storm events are forecast to bring to the area, strong southerly wind and light snowfall. Expect continued formation of fresh wind slabs and building 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 have scoured windward areas and redistributed past storm snow into wind slabs in lee areas. Wind slab depth has been reported up to 50 cm in depth.

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 snowpack remains weak and heavily faceted.

Weather Summary

Saturday night

Cloudy with very light snowfall, a trace to 1 cm of accumulation. Alpine temperatures are cooling to -12 °C. Ridgetop wind northwest 40 km/h gusting to 60 km/h. The freezing level is expected to fall to the valley bottom.

Sunday

Clearing with clouds beginning in the late afternoon. very light snowfall, trace amounts of accumulation. Alpine temperatures -10 °C. Ridgetop wind northwest 60 km/h easing to 30 km/h. Freezing level 200 m.

Monday

Cloudy with snowfall, 5 to 10 cm of accumulation. Alpine temperatures reach a high of -4 °C. Ridge wind southwest 60 km/h gusting to 100 km/h. Freezing level 700 m.

Tuesday

Cloudy with snowfall, 1 to 5 cm of accumulation. Alpine temperatures reach a high of -4 °C. Ridge wind southwest 30 km/h gusting to 75 km/h. Freezing level 700 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.