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Avalanche Forecast

Archived

Jan 26th, 2020–Jan 27th, 2020

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

Regions

Northwest Inland.

Triggering avalanches remains possible where strong winds have drifted the recent snow into slabs at higher elevations. Seek out sheltered slopes or monitor for these conditions if travelling in wind-exposed areas.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

Sunday night: Cloudy, 2-5 cm of snow, moderate southwest winds, gusting strong, alpine temperature -4 C, freezing level around 600 m.

Monday: Mostly cloudy, 2-5 cm of snow, moderate southwest winds, alpine high temperature -6 C, freezing level around 500 m.

Tuesday: Mix of sun and cloud, a trace of snow, moderate southwest winds, alpine high temperature -5 C, freezing level at valley bottom.

Wednesday: Cloudy, 5-15 cm of snow, strong southwest wind, alpine high temperature -2 C, freezing level around 600 m.

Avalanche Summary

Several natural and human-triggered wind slab avalanches were reported over the weekend (up to size 2.5). Over the past week, there have been reports of storm slabs (up to size 2) releasing on a faceted interface from mid-January (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 activity at this interface was Monday January 13th.

Snowpack Summary

South winds have drifted the recent 15-30 cm of snow (up to 50 cm in the Howson area) into slabs near and above tree line. These slabs sit on previously scoured surfaces from the arctic outflow winds or a weak layer of facets.

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 in the last few weeks. These larger avalanches have been specific to lee and cross-loaded features in the alpine.

Terrain and Travel

  • Expect slab conditions to change drastically as you move into wind exposed terrain.
  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.

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.