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Avalanche Forecast

Archived

Jan 19th, 2022–Jan 20th, 2022

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

Regions

Kootenay Boundary.

Reactive storm slabs will build on Thursday with new snow, strong wind, and warmer temperatures. 

Be mindful of the lingering deep persistent slab problem. Caution on shallow snowpack areas and thin to thick steep rocky zones.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Thursday Night: Increasing cloud cover later in the evening with some new snow forecast up to 5 cm. Ridgetop wind light from the southwest and alpine temperatures near -5. 

Thursday: Snow 5-15 cm accompanied by moderate ridgetop wind from the southwest. Alpine temperatures warming to near -2 and freezing levels 1300 m.

  

Friday: Mostly cloudy with sunny periods. Ridgetop winds moderate from the northwest. Alpine temperatures near -5 and freezing levels 1000 m.

Saturday: Cloudy with sunny periods. Alpine temperatures near -2 with light northwest winds. Freezing levels near 1100 m.

Avalanche Summary

No new reports by Wednesday afternoon. 

During the warm previous storm, mid-last week, a large widespread avalanche cycle occurred with most avalanches releasing within the storm snow and some on Jan 11 surface hoar layer. Strong solar radiation and warm temperatures were also at play after the storm, producing numerous avalanches at all elevations and scouring avalanche paths to the ground in places.

We have not heard reports of persistent slab avalanches for the last 10 days when we saw numerous sizes 2 to 3 avalanches releasing on the early December facet/crust layer. Although the activity on this layer has tapered off, it still remains a concern as it is extremely difficult to forecast.

Snowpack Summary

The new snow forecast for Thursday may have a poor bond to the plethora of snow surfaces. These older surfaces consist of wind-scoured on westerly slopes to soft snow and new surface hoar development. Around 1900 m and below, a crust is now capping the upper 30 cm of the snowpack which has settled significantly with the past mild temperatures. The crust varies from thin/breakable to thick/supportive, according to the aspects and elevation. Below this, feathery surface hoar and additional melt-freeze crusts exist. Lower elevations have gone through a melt-freeze cycle with past freezing levels up to 1500m.

The early December crust/facet layer has been responsible for sporadic but very large, persistent slab avalanches over the past month. The crust is now buried 120-200 cm deep except in thin, wind-affected areas near ridgetops where most of the recent avalanches have been triggered.

Terrain and Travel

  • Watch for fresh storm slabs building throughout the day.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and unsupported terrain features.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.