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Avalanche Forecast

Archived

Apr 21st, 2025–Apr 22nd, 2025

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kitimat, Nass, Rupert, Seven Sisters, Shames, Howson.

Recently formed wind slabs may be reactive to human triggering.

Data is very sparse this time of year. During periods of uncertainty, a cautious approach is always recommended.

Confidence

Low

Avalanche Summary

No new avalanches have been reported recently, but observations have been very limited in this region.

Snowpack Summary

A widespread surface crust formed following last week's warming event. At upper elevations, moderate to strong southwest winds will continue to redistribute new snow in exposed terrain.

There are three notable weak layers from February and March in the middle of the snowpack. These layers have recently gone dormant and are not expected to pose a hazard under the current conditions.

Weather Summary

Monday night

Cloudy with up to 5 cm of new snow. 30 to 50 km/h northwest ridgetop wind. Treeline temperature -4 °C. Freezing level 700 m.

Tuesday

Cloudy with up to 5 cm of new snow. 30 to 50 km/h northwest ridgetop wind. Treeline temperature -3 °C. Freezing level rises to 1100 m.

Wednesday

Mostly cloudy with light flurries. 20 to 30 km/h southwest ridgetop wind. Treeline temperature +1 °C. Freezing level rises to 1500 m.

Thrusday

A mix of sun and cloud. 30 to 50 km/h south ridgetop wind. Treeline temperature +2 °C. Freezing level rises to 1900 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Watch for newly formed and reactive wind slabs as you transition into wind-affected terrain.
  • Be alert to conditions that change with elevation, aspect, and exposure to wind.
  • Pay attention to cornices and give them a wide berth when traveling on or below ridges.

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.