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 29th, 2024–Mar 1st, 2024

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

Regions

North Columbia, South Columbia, Esplanade, Jordan, North Selkirk, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Retallack, Whatshan.

Dangerous avalanche conditions persist at all elevations. The snowpack will remain primed for rider triggering as natural avalanches taper off.

Confidence

High

Avalanche Summary

Numerous natural and rider-triggered storm slab and persistent slab avalanches size 1 to 3.5 with wide propagations have been reported the past few days at all elevations. Persistent slabs have been reported on all aspects and 60 to 100 cm deep. Some of the rider-triggered avalanches resulted in partial or full burials and many were remotely triggered (from a distance).

Expect storm and persistent slab avalanche activity to continue.

Snowpack Summary

70 to 110 cm of recent snow sits on a variety of layers, including surface hoar in wind-sheltered terrain, weak facets, or a hard melt-freeze crust on sun-exposed south and west-facing slopes. A plethora of recent avalanche observations indicate the fresh snow is not bonding well to these layers. Gusty southerly winds have stripped fresh snow in exposed areas and loaded lee features with over 130 cm of wind-blown snow.

A thick and hard widespread crust that formed in early February is buried 60 to 120 cm deep and is found up to around 2400 m. This crust may have a layer of facets above it and is a troublesome avalanche layer.

The remainder of the snowpack is settled.

Weather Summary

Thursday Night

Cloudy with 5 to 15 cm of snow for most areas, and hotspots of up to 30 cm focused on areas south of Hwy 1. 15 to 30 km/h southwest ridgetop wind. Treeline temperature -10 °C. Freezing level dropping to valley bottom.

Friday

Mostly cloudy with flurries and isolated sunny breaks, up to 10 cm of snow. 15 to 40 km/h southwest ridgetop wind. Treeline temperature -5 °C. Freezing level 900 m.

Saturday

Mostly cloudy with sunny breaks and isolated flurries. 15 to 30 km/h southwest ridgetop wind. Treeline temperature -6 °C. Freezing level 600 m.

Sunday

Mostly cloudy with scattered flurries, up to 10 cm of snow. 15 to 30 km/h southwest ridgetop wind. Treeline temperature -8 °C. Freezing level valley bottom.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Only the most simple non-avalanche terrain free of overhead hazard is appropriate at this time.
  • Remote triggering is a concern, watch out for adjacent and overhead slopes.
  • Be aware of the potential for surprisingly large avalanches due to deeply buried weak layers.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.

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.