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Avalanche Forecast

Archived

Jan 23rd, 2020–Jan 24th, 2020

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

Regions

Kootenay Boundary.

Triggering avalanches remains likely where new snow and wind has formed storm slabs, especially at higher elevations.

Confidence

High - The number, quality, or consistency of field observations is good, and supports our confidence.

Weather Forecast

THURSDAY NIGHT: Frontal system crossing the region with 10 cm of new snow, moderate wind from the south, freezing level around 1500 m with alpine temperatures around -3 C.

FRIDAY: Scattered flurries with another 10 cm of snow, moderate wind from the southwest, freezing level around 1500 m with alpine high temperatures around -1 C.

SATURDAY: Cloudy with light flurries, light wind from the southwest, freezing level around 1200 m with alpine high temperatures around -3 C.

SUNDAY: Mostly cloudy, light wind, alpine high temperatures around -5 C.

Avalanche Summary

The current storm has formed fresh slabs at higher elevations, as evident from this MIN report on Thursday of a skier triggered avalanche at Kootenay Pass. This avalanche was triggered on a south aspect at treeline and ran for a long distance above the recently buried crust.

No persistent slab avalanches have been observed since January 14, suggesting deep weak layers have become difficult to trigger under the current conditions.

Snowpack Summary

With 15-30 cm of snow over the past three days and another 10-20 cm in the forecast for Friday, expect fresh storm and wind slabs. This snow sits above a thin crust layer that formed last weekend. We have been tracking two layers over the past month: a layer of surface hoar buried 80-120 cm below the surface and faceted crystals and crusts near the bottom of the snowpack in certain parts of the region (especially western areas such as the Rossland Range and Boundary region). Both of these layers have shown signs of being less reactive over the past 10 days.

Terrain and Travel

  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Be especially cautious as you transition into wind affected terrain.

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.