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Avalanche Forecast

Archived

Jan 25th, 2020–Jan 26th, 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 unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
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. Stay alert and monitor for these conditions if travelling in these areas.

Confidence

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

Weather Forecast

Saturday night: Partly cloudy, scattered flurries with trace accumulations, strong southwest winds, alpine temperature -5 C, freezing level dropping to 500 m.

Sunday: Mostly cloudy, a trace of new snow, moderate southwest winds, alpine high temperature -3 C, freezing level around 500 m.

Monday: A trace of new snow. Moderate south to southwesterly winds. Alpine high -4 C. Freezing level around 500 m.

Avalanche Summary

A few small, human-triggered wind slab avalanches were reported on Friday. Earlier in the week, there were reports of storm slabs releasing naturally (see this MIN report).

Last weekend, a natural storm cycle was observed at treeline and below. Slabs were soft and thin but propagated widely resulting in avalanches up to size 2. They ran on the faceted interface buried January 17th.

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

Southerly winds have formed fresh wind slabs with the 15-30 cm (up to 50 cm in the Howson area) of recent snow. These slabs sit on previously scoured surfaces from the arctic outflow winds. In wind sheltered areas at treeline and below, the recent snow sits on a 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.