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Avalanche Forecast

Archived

Jan 29th, 2021–Jan 30th, 2021

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural and human triggered avalanches likely.

Regions

Kootenay Boundary.

Friday's observations show storm slabs a bit tougher to initiate, but they're still releasing with light triggers. Keep your guard up at all elevations. This is a widespread, reactive avalanche problem.

Confidence

High -

Weather Forecast

FRIDAY NIGHT: Cloudy with scattered flurries bringing up to 5 cm of new snow. Light to moderate southwest winds, increasing into the morning.

SATURDAY: Cloudy with continuing scattered flurries and up to 5 cm of new snow, increasing overnight. Light to moderate southwest wind, increasing over the day and becoming strong overnight. Alpine high temperatures around -7.

SUNDAY: Continuing snowfall bringing 10-20 cm of new snow, with new snow totals reaching about 20-40 cm, continuing overnight. Moderate to strong south winds. Alpine high temperatures around -4 with freezing levels rising to about 1400 metres.

MONDAY: Cloudy With continuing snowfall bringing 15-20 cm of new snow and 3-day snow totals to around 50-80 cm, easing overnight. Moderate to strong south winds, easing overnight. Alpine higfh temperatures around -4 with freezing levels to about 1400 metres.

Avalanche Summary

Preliminary reports from Friday show storm slabs reacting to skier traffic a bit more stubbornly, but still producing 40-50 cm-deep avalanches. This pattern will likely persist through Saturday before forecast weather takes things up a notch.

Observations from Thursday included numerous storm slab releases in the size 1-2 range (small to large). These included recent natural avalanches as well as ski cut and explosives results. All aspects and elevations were well represented, with our latest weak layer of surface hoar from late January, about 20-45 cm deep in reports, identified as a primary failure plane. Observations of the alpine are still limited.

With a bit more new snow adding to the avalanche problem discussed above, thick storm slabs are expected to remain sensitive to human triggering on Saturday.

Snowpack Summary

About 10 cm of new snow is expected to accumulate by the end of the day on Saturday. This will add to 25-50 cm of snow from a midweek storm which sits on firm wind slabs in exposed areas, on a melt-freeze crust in many areas around treeline and below treeline, on a sun crust on steep south-facing slopes, and on large surface hoar in sheltered areas.

There are potentially several more layers of surface hoar in the upper snowpack, with the most notable one down about 50-70 cm. This layer was buried in early January.

A couple of crusts surrounded by weak faceted grains are buried deep within the snowpack. The upper layer is 80 to 130 cm deep and the lower one is near the ground. 

Terrain and Travel

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

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.