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

Feb 25th, 2025–Feb 26th, 2025

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

Regions

North Columbia, South Columbia, Jordan, North Selkirk, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, Retallack, Valhalla, Whatshan.

Choose mellow terrain, and avoid lingering under steep slopes, especially if it's sunny.

Human-triggered avalanches will likely remain a threat over the next few days.

Confidence

Moderate

Avalanche Summary

On Monday, widespread small to large (up to size 3) natural and human triggered avalanches continued to be reported. They were most common on north through southeast facing treeline terrain.

Some involved just the recent storm snow, but others failed up to 100 cm deep, on a weak layer buried in late January.

Some avalanches at treeline and below became wet and entrained a lot of debris.

We expect similar avalanches to occur on Wednesday.

Snowpack Summary

30 to 50 cm of settling snow sits atop layers of surface hoar in sheltered terrain and a thin crust on sun-affected slopes.

Below these layers, the upper snowpack is largely faceted and poorly bonded with another layer of surface hoar in sheltered terrain and a thin crust on sun-affected slopes. This layer, buried in late January, varies in depth but generally exists within the upper 100 cm of snow.

The mid and lower snowpack is generally well-settled and strong.

Weather Summary

Tuesday Night

Cloudy with up to 2 cm of snow. 10 to 25 km/h west ridgetop wind. Treeline temperature -4 °C. Freezing level 1400 m.

Wednesday

Mostly cloudy in the morning, clearing in the afternoon. 10 to 20 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level rising to 1750 m.

Thursday

Mostly cloudy with scattered flurries, as much as 5 cm in some places. 30 to 40 km/h southwest ridgetop wind, lighter on the east side of the forecast area. Freezing level falling to 1000 m overnight, rising to 1800 m.

Friday

Mostly sunny. 10 to 20 km/h southwest ridgetop wind. Freezing level falling to near valley bottom overnight, rising to 2250 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Keep in mind that human triggering may persist as natural avalanches taper off.
  • Use conservative route selection and resist venturing into complex terrain.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • The more the snowpack warms up and weakens, the more conservative your terrain selection should be.

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.