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Avalanche Forecast

Archived

Jan 9th, 2021–Jan 10th, 2021

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

Regions

North Columbia.

Watch for wind slabs that may remain sensitive to human triggers and keep in mind the lingering potential for large and destructive persistent slab avalanches. 

Confidence

Moderate - Uncertainty is due to how the snowpack will react to the forecast weather.

Weather Forecast

Saturday night: Increasing cloud, light to moderate southeast wind, freezing level valley bottom.

Sunday: Flurries, trace, moderate southeast wind, alpine high -8, freezing level 700 m.

Monday: Flurries, 5-10 cm, moderate southwest wind, alpine high -6, freezing level 1200 m.

Tuesday: Snow, 10-20 cm, strong southwest wind, alpine high -6, freezing level 1200 m.

Avalanche Summary

We have received few reports of avalanche activity in the region since the mid-week storm slab avalanche cycle produced natural avalanches size 2-3.5. But with similar snowpack structure and recent weather patterns to neighboring Glacier National Park and South Columbia regions, we suspect that recent avalanche activity has been similar, but has gone unreported due to less backcountry traffic. 

Natural storm slab avalanches size 1.5-2.5 have been reported in GNP as recently as Friday. Notable avalanches in South Columbia include several skier triggered incidents around size 2 in the RMR slackcountry and a few natural persistent slab avalanches size 2.5-3 on northerly aspects in the alpine running on the early December persistent weak layer. See South Columbia avalanche summary for details.

Snowpack Summary

Variably wind affected surfaces can be found at upper elevations. Around 50-80 cm of recent snow sits on a weak layer of surface hoar that was buried around Christmas at and below treeline.

A couple of persistent weak layers buried in early/mid-December are buried 90-150 cm down. Generally, they can be found as a layer of surface hoar above in close proximity to a crust/surface hoar layer. The form and distribution of these layers are highly variable and conditions may differ significantly from one valley to the next. 

Terrain and Travel

  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Avalanche hazard may have improved, but be mindful that deep instabilities are still present.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

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.

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.