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Avalanche Forecast

Archived

Jan 2nd, 2021–Jan 3rd, 2021

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.
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.

Regions

South Coast Inland.

New snow and wind will be forming fresh and reactive storm slabs. Choose simple terrain and avoid overhead hazard.

A complex snowpack has produced large avalanches and several incidents in the last week, including a fatal avalanche near Pemberton on Monday.

Confidence

Moderate - We are confident about the likelihood of avalanche activity, what is less certain are their possible size. Uncertainty is due to how buried persistent weak layers will react with the forecast incoming weather.

Weather Forecast

Saturday night: Snow, 10-20 cm in most areas, lighter snowfall in areas north of Pemberton, moderate to strong southwest wind, freezing level 700 m.

Sunday: Flurries, 5-10 cm, moderate to strong southwest wind, alpine high temperature near -7, freezing level 1200 m.

Monday: Flurries, up to 5 cm, light southwest wind, alpine high temperature near -3, freezing level 1000 m.

Tuesday: Flurries, up to 5 cm, moderate southwest wind, alpine high temperature near -6, freezing level 1000 m.

Avalanche Summary

Avalanches are expected to be widespread on Sunday. 

Numerous storm slab avalanches, natural and explosive triggered size 2-4 (!) were reported on Friday and Saturday. 

There was a fatal avalanche north of Pemberton in the Railroad Pass area on Monday that resulted in two fatalities. It was reported to be a size 2 persistent slab avalanche on a west aspect, around 1650 m. The RCMP press release can be viewed here and the Avalanche Canada report can be found here.

A size 2 avalanche was triggered on Monday by a skier on a northwest aspect in the alpine on Mt. Matier (Duffey). The avalanche occurred on a northwest aspect and was likely a wind slab avalanche. It carried the skier over cliffs resulting in several injuries. A MIN report detailing this incident can be found here. 

A few persistent slab avalanches were reported last week, mostly in the north of the region near the Hurley, but also near Allison Pass. They were triggered by riders, heavy machinery, and naturally. The slabs were generally 60 to 90 cm deep, around 2000 m, and released on the weak layers described in the snowpack summary.

Snowpack Summary

15-30 cm of new snow overnight Saturday and over the day Sunday will bring recent storm snow totals to around 60-100 cm. This snow may be sitting on surface hoar below treeline. Large snowfall amounts combined with strong southwest winds will most likely form widespread and reactive storm slabs.

A melt-freeze crust from early December is found around 80 to 180 cm deep in the snowpack. This crust may have surface hoar or sugary faceted grains sitting above it. This persistent weak layer is most prevalent in the north (e.g., Duffey Lake, Hurley) and found to a lesser extent in the south of the region.

The remainder of the snowpack is generally well settled.

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • 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.