Avalanche forecast

Banff Yoho Kootenay

Jan 31 – Feb 1, 2022
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Avalanche danger

Tue
Wed
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
2 · Moderate

Highlights

An upslope storm (NE flow, reverse winds) starts tonight giving us a 10-15 cm refresh of snow by Monday afternoon with a cooling trend. Expect small fresh windslabs and note the date (Jan 30), because a new weak layer is getting buried now.

Avalanche problems

  • Wind Slabs

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

    These are new windslabs formed overnight on Sun and associated with the new snow. We expect them to be thin (ie: < 25 cm) but very sensitive to triggers as they bury a new weak layer. This is different from the windslabs described in previous days.

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Unlikely - Possible
    Size
    2–3

    This problem represents both the Dec. 2nd crust/ facet layer (treeline and below) and the late December facet layer. Lots of variation in the sensitivity ranging from reactive sudden collapse to no results depending on location, aspect and elevation.

Weather Forecast

Winds shift to a NE upslope flow overnight on Sunday with 10 cm expected by Monday morning under cooling temperatures as a cold front crosses the area making for blustery conditions. This should clear out by the end of Monday, leaving a maximum of 15 cm of snow in its wake. Temperatures continue to drop until Wednesday morning.

Snowpack Summary

10cm of new snow under an upslope flow will produce small, fresh windslabs and surface instabilities that bond poorly to the underlying surface of crust and facets (hint: new weak layer getting buried). Expect easy triggering of thin slabs. This storm is unlikely to wake up the deep facets, but they continue to lurk anywhere from 60-100 cm deep.

Avalanche Summary

No new avalanches observed or reported on Sunday. Over the past week we have received reports and observed a few avalanche to size 3 on the persistent weak layer. All of these avalanches were triggered by large loads (cornice).

Confidence

Regions covered