Avalanche forecast

North Columbia

Apr 9 – 10, 2022Avalanche Canada
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Avalanche danger

Mon
Tue
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
1 · Low

Highlights

Recent strong southwesterly winds formed wind slabs on lee aspects at treeline and above.

Use high points in the terrain such as ridges or ribs to avoid areas of wind-loaded snow. 

Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2

    Recent strong southwesterly winds formed wind slabs on lee aspects at treeline and above.

    Use high points in the terrain such as ridges or ribs to avoid areas of wind-loaded snow. 

Confidence

High -

Weather Forecast

Saturday night: Partly cloudy / Light northwest wind / Low of -11 / Freezing level valley bottom.

Sunday: Mix of sun and cloud with convective flurries, 0-3 cm / Light north wind / High of -3 / Freezing level 1100 m.

Monday: Mix of sun and cloud / Light east wind / High of -4 / Freezing level 900 m.

Tuesday: Mix of sun and cloud / Light east wind / High of -6 / Freezing level valley bottom.

Avalanche Summary

A couple natural and skier triggered wind slab avalanches up to size 2.5 were reported on northeast to southeast aspects at treeline and above on Friday.

Snowpack Summary

5-15 cm of new snow buries a breakable melt-freeze crust that exists on all aspects to at least 2200 m.

Recent strong southwesterly winds formed wind slabs on lee aspects at treeline and above.

Recent avalanches have been failing on a melt-freeze crust down 60-80 cm. Occasionally, these avalanches have stepped-down to a rain crust formed in early December which resulted in some very large avalanches. 

These large events are most likely to occur during periods of warming when freezing levels reach roughly 2500 m or higher.

Cornices are very large and exposure to slopes beneath them should be minimized, especially if the weather is sunny, warm, or windy.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Wind slabs may be poorly bonded to the underlying crust.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

Regions covered