Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 22nd, 2023–Jan 23rd, 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.

Although avalanche activity on buried weak layers has subsided, the snowpack is still weaker and thinner than usual. This is best managed by choosing conservative terrain.

Confidence

Moderate

Avalanche Summary

Although avalanche activity has subsided, reported avalanche activity over the previous 2 weeks indicates the potential of the deeper weak layers buried in the snowpack. While this is not recent activity or an easily predictable trend - it continues concern for these layers. The Hurley has been the bulls-eye for avalanche activity on persistent weak layers in the middle and bottom of the snowpack.

Please continue to share any observations or photos on the Mountain Information Network.

Snowpack Summary

The region's generally weak snowpack structure remains.

Up to 10 cm of storm snow is can be found over wind affected surfaces at higher elevations, and over a crust at lower elevations.

A weak layer that formed in late December can be found 50-70 cm deep. In the Hurley and Birkenhead areas it may present as surface hoar sitting on a crust and can be found between 1700 and 1900m in elevation. The crust varies in thickness with terrain and elevation; in many places it's more of a soft and weak section of the snowpack.

There is a widespread weak layer of facets and depth hoar at the bottom of the snowpack. Snowpack depths around treeline are about 150 cm deep.

Weather Summary

Sunday Night

Mainly cloudy with isolated flurries. Light to moderate west and northwest wind. Alpine high of -7 °C. Freezing level around 700 m.

Monday

Mostly clear with light to moderate northwest winds. Freezing levels around 500 m, alpine high of -5 °C.

Tuesday

Mostly clear with light to moderate northwest winds. Freezing levels around 500 m, alpine high of -5 °C.

Wednesday

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Uncertainty is best managed through conservative terrain choices at this time.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

Problems

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.

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.