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Avalanche Forecast

Archived

Jan 31st, 2022–Feb 1st, 2022

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

Regions

Kootenay Boundary.

The recent storm snow is expected to remain touchy on Tuesday, especially in wind loaded terrain and on steep slopes where it overlies surface hoar or a crust.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

Unsettled conditions are expected on Tuesday as Arctic air shifts southward. 

Monday Night: Partly cloudy, moderate NW wind, treeline temperature dropping to around -10 C°.

Tuesday: Snow flurries up to 5 cm in the morning, sunny breaks in the afternoon, light to moderate NW wind, treeline high around -8 C°.

Wednesday: A mix of sun and cloud, light variable wind, treeline high around -10 C°.

Thursday: A mix of sun and cloud, light variable wind, treeline high around -6 C°.

Avalanche Summary

On Sunday, ski cutting triggered three size 1 wind slabs on NE aspects at around 2000 m failing on the Jan 14 SH down 20-30 cm. A skier also triggered a size 1 slab on a NE aspect at around 2100 m failing on the newest surface hoar down 15 cm. Some other small skier triggered slabs were reported failing down 25-35 cm on surface hoar and small loose dry avalanches were observed in very steep terrain. This MIN report suggests the new storm snow was becoming reactive immediately on Sunday in wind loaded terrain, even with only 4-6 cm of new snow. 

Snowpack Summary

Up to 20 cm of new snow has buried a highly variable snow surface which consists of wind affected surfaces in exposed high elevation terrain, a melt freeze crust at lower elevations and on solar aspects extending into the alpine, and/or widespread surface hoar in sheltered areas which is appears to typically be 5-15 mm but could be as large as 20-30 mm in places. 

There are several crusts and surface hoar layers buried 30-60 cm deep. These layers have not been much of a problem recently but may become more reactive with the additional storm loading. 

The early December crust/facet persistent weak layer is down 100-200 cm and has been responsible for sporadic avalanche activity throughout the first half of January. The layer has been mainly dormant in the region for the past couple weeks but still remains a concern. See the most recent forecaster blog for more details on this layer. 

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Wind slabs may be poorly bonded to the underlying crust.
  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.