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

Mar 8th, 2026–Mar 9th, 2026

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

Regions

Coquihalla, Harrison-Fraser, Manning, Skagit.

Wind slabs remain possible following recent snow, wind, and cooling temperatures.

Significant uncertainty remains about how recent rapid weather changes have affected the snowpack.

Confidence

Moderate

  • We are uncertain about how quickly persistent slabs are gaining strength.
  • We are uncertain due to variable freezing levels.

Avalanche Summary

We do not have any recent reports of avalanches, but suspect a natural cycle occurred with recent rain and warm temperatures.

Last weekend (Feb 28/Mar 1), numerous large (up to size 3) avalanches were reported, both natural and human-triggered, all suspected to have failed on a late January crust/facet layer. They were mostly at treeline, although two human-triggered avalanches were in open, alpine, or alpine-like terrain.

Snowpack Summary

Recent precipitation fell as snow at higher elevations and rain at lower elevations, with temperatures cooling significantly over the weekend.

At higher elevations, strong westerly winds accompanied the snow, creating deeper deposits in leeward and cross-loaded terrain. Mid elevations likely have a crust or light snow atop a crust from the recent cooling, while surface snow at lower elevations remains moist or crusty.

On north aspects, 50 to 150 cm below the surface, two persistent weak layers exist (buried in late January and early February) and contain facets over a crust. It remains uncertain whether the recent warm conditions had any effect on the reactivity of these layers.

Weather Summary

Sunday Night
Mostly cloudy. 2 to 8 cm of snow. 50 km/h west ridgetop wind. Treeline temperature -8 °C.

Monday
Cloudy. 3 to 5 cm of snow. 30 km/h southwest ridgetop wind. Treeline temperature -10 °C.

Tuesday
Mostly cloudy. 10 to 20 cm of snow. 40 km/h southwest ridgetop wind. Treeline temperature -10 °C.

Wednesday
Mostly cloudy. 15 to 20 cm of snow. 50 km/h southwest ridgetop wind. Treeline temperature -7 °C.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Approach lee and cross-loaded slopes with caution.
  • Wind slabs are most reactive during their formation.
  • If triggered, wind slabs may step down to deeper layers, causing larger avalanches.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.