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Avalanche Forecast

Archived

Jan 29th, 2020–Jan 30th, 2020

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

Regions

Northwest Inland.

Snow and wind will build increasingly reactive storm slabs and stress a buried weak layer. Seek out simple and sheltered terrain as snow accumulates.

Confidence

Moderate - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather. Uncertainty is due to how buried persistent weak layers will react with the forecast incoming weather.

Weather Forecast

Wednesday night: Flurries, up to 10 cm. Alpine low temperature -10 C. Moderate southwest winds gusting to strong.

Thursday: Snow, 10-15 cm. Alpine high temperature -4 C. Strong gusting to extreme southwest winds. Freezing level rising to 1000 m.

Friday: Flurries and snow, 5-20 cm. Alpine high temperature -3 C. Moderate southwest winds gusting strong to extreme. Freezing level 1000 m.

Saturday: Flurries, 5-15 cm. Alpine high temperature -9 C. Moderate west wind gusting to strong. Freezing level dropping to valley bottom.

Avalanche Summary

Several natural and human-triggered wind slab avalanches were reported last weekend (up to size 2.5). Reports indicate that recent storm and wind slab avalanches have failed on a faceted interface from mid-January that developed with cold temperature prior to the last heavy snowfall (see an example in this MIN report).

There have been reports trickling in over the past month of natural persistent slab avalanches up to size 3 in the Bulkley Valley. These are thought to have been failing on the November crust/facet layer near the ground. The last reported avalanches on this layer were Monday January 13th. Incremental snowfall and mild temperatures have likely promoted a decreasing trend in reactivity for this avalanche problem. 

Snowpack Summary

Incoming snow and strong winds will build a reactive storm slab problem, particularly in wind-exposed areas.

Below the new snow, last week's 25-40 cm of snow accumulation rests on mix of previously scoured surfaces from the arctic outflow winds or a weak layer of facets. The incoming snowfall and wind will add a new load this persistent weak layer, potentially bringing it to its tipping point.

A layer of surface hoar now buried up to 1 m below the surface may also be found at treeline. A deep crust/facet layer lurks at the base of the snowpack. A couple of large avalanches are suspected to have run on this interface earlier in January. These have typically run in alpine terrain, on lee and cross-loaded slopes. While it is promising that last week's snowfall did not trigger avalanches on this deep persistent weak layer, there is lingering uncertainty as to whether this week's weather could meet the threshold. 

Terrain and Travel

  • Storm snow and wind is forming touchy slabs. Use caution in lee areas in the alpine and treeline.
  • Expect slab conditions to change drastically as you move into wind exposed terrain.
  • Watch for avalanche hazard to increase throughout the day.
  • 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.

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.