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Avalanche Forecast

Archived

Jan 27th, 2022–Jan 28th, 2022

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

Regions

Northwest Coastal.

Use extra caution around large slopes and thin areas at treeline. There is uncertainty in how the mid January surface hoar layer will respond to the incoming weather.

Confidence

Low - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Thursday night: freezing level will fall to 500m with moderate to strong south winds in the alpine. Light snow starting around midnight.

FRIDAY: Storm arrives with cloudy skies and up to 10mm of precipitation. Moderate to strong wind from the south, freezing level fluctuates between 500 m and 1000 m.

SATURDAY: Stormy weather continues with another 15cm of snow, strong wind from the south, freezing level fluctuates between 500 m and 1000 m.

Sunday: some light flurries with light to moderate southwest winds. High of -2 at 900m.

Avalanche Summary

Warm sunny weather earlier this week has resulted in a few loose wet and glide slab avalanches. The most concerning avalanche activity has been a string of persistent slab avalanches over the past week. These have occurred on a 30-50 cm deep layer of surface hoar in southern parts of the region around Terrace and Stewart. This has included both natural avalanches and human-triggered avalanches. The photos of the avalanche in this MIN report at Clague are good examples of the type of treeline elevation terrain where this problem can be found. We are uncertain whether the persistent slab problem will remain reactive after the melt freeze cycle tapers off.

Snowpack Summary

As the storm arrives early Friday morning new wind slab and storm slabs could develop over old refrozen surfaces.

The snow surface has recently undergone a spring-like melt-refreeze pattern. The snowpack is likely capped by a hard crust in most areas except high north facing terrain. Below this is a surface hoar layer burried 30 to 50cm deep and could still be triggered at treeline in the Terrace and Stewart areas.

Terrain and Travel

  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Wind slabs may be poorly bonded to the underlying crust.

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.

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.