Avalanche forecast

Northwest Inland

Jan 28 – 29, 2016Avalanche Canada
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Avalanche danger

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

Highlights

In the west of the region where recent accumulations were the greatest, new wind slabs are expected to be deeper and more reactive

Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely
    Size
    1–3
    Continued strong winds and new snow have likely formed reactive wind slabs at treeline and in the alpine. New winds slabs are expected to be larger on the west side of the region where recent accumulations were the greatest.
  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–3
    New snow has been slowly accumulating over a layer of facets and surface hoar. In some areas, recent rain may have destroyed the layer. In other areas, the overlying slab may be primed for human triggering.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

On Friday expect 5-10cm on new snow, strong southerly winds and freezing levels at about 800m. On Saturday, the region will see another 5cm of new snow with mainly overcast skies forecast for Sunday. Winds for the weekend will be mainly light from the north while freezing levels hover around 500m.

Avalanche Summary

There are very few recent observations from the region. Light to locally moderate amounts of new snow and extreme southwest winds likely sparked a new round of wind slab activity. Recent rain may have also promoted loose wet avalanche activity at treeline and below.

Snowpack Summary

Since Monday night generally light amounts of new snow fell in the mountains around Smithers while closer to 40 cm fell in areas further west. Strong to extreme winds have likely redistributed much of this new snow into reactive wind slabs at higher elevations while surfaces at treeline and below are likely now moist or refrozen due to rising freezing levels during the system. There is a notable persistent weakness of buried surface hoar in many places, generally found between 30 and 80 cm deep. Wind and milder temperatures may have helped to promote slab development in the snow overlying this interface. In other areas, rain may have destroyed the layer. Stay tuned to signs of instability like recent avalanches, whumpfing, and shooting cracks. The mid pack that was reported to be well settled may have now facetted in the shallower areas, and the deeper basal layers are almost certainly facetted and weak.

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