Avalanche forecast

South Columbia

Jan 5, 2018Avalanche Canada
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Archived · expired 9 years ago

Avalanche danger

Sat
Sun
Alpine
2 · Moderate
Treeline
3 · Considerable
Below
2 · Moderate

Highlights

A weak layer is buried at a depth prime to human triggering.  As the overlying snow settles and forms a slab, destructive avalanches will likely result.  Cautious route finding is advised, particularly at treeline elevations.

Avalanche problems

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2
    Around 50 to 70 cm of snow sits above a touchy weak layer.  As this snow settles and gains slab properties, a dangerous slab that is easily triggered will likely form.
  • Loose Dry

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–2
    A human could trigger loose snow avalanches in steep terrain.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

FRIDAY: Mostly cloudy with light snowfall, light southwesterly winds, freezing level near valley bottom.SATURDAY: Cloudy with light snowfall, accumulation 5-10 cm, light southerly winds, freezing level near valley bottom.SUNDAY: Cloudy with light snowfall, accumulation 2-5 cm, light southwesterly winds, freezing level near valley bottom.

Avalanche Summary

On Wednesday, skiers triggered small avalanches on the December 15 layer below and at treeline elevations on southerly aspects.  Small, loose avalanches were noted on steep southerly slopes. Reactivity of the persistent slab is likely to increase with warmer temperatures below treeline as the snow forms slab properties.

Snowpack Summary

A warming trend is creating a dangerous slab above buried weak layers in some areas.  Numerous persistent weak layers exist in the snowpack.  Dry snow overlies two layers composed of weak and feathery surface hoar, with the deeper layer (December 15) buried 50 to 70 cm.  This layer is found most often around and below treeline.  As the overlying dry snow becomes more cohesive and forms a slab, this layer has the potential to create easily-triggerable destructive slab avalanches.  Where and when this will occur is tricky to predict and even professionals are scratching their heads about it. It is a good time for conservative decision-making.The snow surface is variable, consisting of dry snow on shaded aspects, a sun crust on steep solar aspects, and wind effect in exposed alpine and treeline locations.Deeper in the snowpack at depths of about 90 to 150 cm, a rain crust from November is producing variable snowpack test results, from sudden fracture characters to no result.  This layer is considered dormant for now, but could be triggered where the snowpack is thin.If you have any recent observations, please share them through the Mountain Information Network.

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