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 31st, 2024–Feb 1st, 2024

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

Regions

North Rockies, Sugarbowl, East Kakwa, Kakwa, McGregor, Pine Pass, Renshaw, Robson, Tumbler.

Until cold temperatures lock in this warm and wet snowpack, dangerous avalanche conditions and poor riding quality will exist.

Human triggered avalanches are possible.

Confidence

Low

Avalanche Summary

On Tuesday, numerous wet loose and wet slab avalanches were reported up to size 2. Sunday and Monday saw a natural avalanche cycle with avalanches on all aspects and elevations to size 3.

A fatal avalanche involving one snowmobiler occurred in the Hasler riding area last Saturday. The avalanche was triggered in a wind-loaded east-facing chute feature at treeline and ran approximately 250 m. For more details on this incident, see the Fatal Avalanche Incident report.

Snowpack Summary

High freezing levels and rain have moistened the surface snow to 2500 m and wet, rain-saturated snow exists up to 2200 m.

A weak layer of facets exist down 30 to 60 cm and a prominent crust down 40 to 100 cm. The crust is reported to extend up to 1900 m in the Cariboos and up to 1800 m around Pine Pass. The stress of the new load (warm, wet upper snowpack) has produced large avalanches possibly failing on these layers.

In areas east of the Divide the snowpack is shallow and faceted with depths of 60 to 100 cm around treeline.

Weather Summary

Wednesday Night

Cloudy, treeline temperatures near 3°C, south alpine wind 30 gusting to 55 km/h, freezing level around 2000 m.

Thursday

Mostly cloudy with rain/snow expected 4 to 7 mm, southwest alpine wind 30 to 40 km/h, freezing level around 1900 m.

Friday

Cloudy with light rain/snow, alpine temperatures near 1°C, southeast alpine wind 20 to 30 km/h, freezing level rising to 1600 m.

Saturday

Mix of sun and cloud, treeline temperatures near -5°C, southeast alpine wind 25 km/h, freezing level valley bottom.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Make conservative terrain choices and avoid overhead hazard.
  • A moist or wet snow surface, pinwheeling and natural avalanches are all indicators of a weakening snowpack.
  • Be aware of the potential for surprisingly large avalanches due to deeply buried weak layers.

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.

Wet Slabs

Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.