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Avalanche Forecast

Archived

Jan 3rd, 2023–Jan 4th, 2023

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, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

South Coast Inland, Birkenhead, Duffey, South Chilcotin, Stein, Taseko.

Continue to assess the snowpack as you mmove through terrain. rider triggerable wind slabs could still be found. Smaller avalanches have the potential to step down to deeper layers resulting in very large avalanches. The snowpack in this region is unusually shallow and fragile.

Confidence

Moderate

Avalanche Summary

No new avalanches reported in the last couple days in the region.

Please continue to post your observations and photos to the Mountain Information Network.

Snowpack Summary

Ongoing southerly winds have scoured south facing terrain in the alpine and formed wind slab in specific north facing features. 20 to 40cm of recent snow sits over a crust formed near the end of December. This crust gets thinner and less supportive as you gain elevation.

In the mid-snowpack, a weak layer of surface hoar from early December has been observed down 80 to 100 cm. This layer is most prevalent in shaded and sheltered areas.

The lower snowpack consists of weak, sugary crystals of facets and depth hoar. This basal weakness remains a concern.

Snowpack depths remain highly variable, roughly 50 to 200 cm at treeline.

Weather Summary

Tuesday night

trace amounts of new snow expected. Light to moderate southerly winds and a low of -12 at 1800m.

Wednesday

A mix of sun and cloud with the possibility of light flurries bringing trace amounts of new snow. Moderate to strong easterly winds and freezing levels around 800m.

Thursday

Cloudy with flurries bringing up to 5cm of new snow. Moderate to strong southeast winds and freezing levels rising to 1200m.

Friday

Cloudy with flurries bringing around 5cm of new snow. Strong southerly winds. Freezing level around 1400m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
  • Be mindful that deep instabilities are still present and have produced recent large avalanches.
  • Avoid shallow snowpack areas, rock outcroppings and steep convex terrain where triggering is most likely.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.

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.