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Avalanche Forecast

Archived

Jan 6th, 2020–Jan 7th, 2020

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

Regions

Kootenay Boundary.

Intense stormy conditions are expected for Tuesday. Natural and human-triggered avalanches will be very likely to occur and they could reach the valley bottom. Travel in avalanche terrain is not recommended.

Confidence

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

MONDAY NIGHT: Cloudy with snowfall, accumulation 15 to 30 cm, light to moderate west wind, alpine temperature -5 C, freezing level 1000 m.

TUESDAY: Cloudy with snowfall, accumulation 25 to 35 cm, moderate to strong southwest wind, alpine temperature -3 C, freezing level 1400 m.

WEDNESDAY: Morning snowfall and afternoon clearing, accumulation 20 to 30 cm, light northwest wind, alpine temperature -6 C, freezing level 1000 m.

THURSDAY: Mix of sun and cloud, light northwest wind, alpine temperature -12 C, freezing level below valley bottom.

Avalanche Summary

Many storm slab avalanches were triggered by skiers and explosives on Monday. The avalanches were generally large (size 1.5 to 2.5).

Avalanche activity is expected to increase through the night and on Tuesday as the storm snow accumulates. Storm slab avalanches will be very likely to be triggered and they may step down to deeper weak layers, forming very large avalanches.

Snowpack Summary

40 to 60 cm of snow is forecast to accumulate Monday night into Tuesday, falling with strong west wind. Storm slabs will quickly develop and be especially touchy in lee terrain features. Below the rain-snow line, loose wet avalanches are likely to prevail.

This snow is loading multiple buried weak layers of feathery surface hoar found 50 to 150 cm in the snowpack. The base of the snowpack is also weak in parts of the region, where it consists of sugary faceted snow around a melt-freeze crust.

This fundamentally unstable snowpack structure remains a concern, as it is capable of producing large and destructive avalanches. It is possible that storm slab avalanches could step down to these deeper layers or the layers could be triggered in areas where the snowpack is relatively thin.

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • If triggered, storm slabs in-motion may step down to deeper layers and result in very large avalanches.
  • Avoid traveling in runout zones. Avalanches have the potential to run to the valley floor.

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.