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Avalanche Forecast

Archived

Dec 10th, 2021–Dec 11th, 2021

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

Regions

North Columbia.

New snow and wind are forming touchy slabs. A weak layer in the upper snowpack means slab avalanches can be larger than expected. Having the skills to recognize and avoid avalanche terrain will be critical to managing your risk on Saturday. 

Confidence

High - A small change in the upper snowpack could dramatically change avalanche conditions.

Weather Forecast

Friday night: 5-15 cm of new snow. Strong to extreme southwest wind. Freezing level climbing to 700 m.

Saturday: 10-15 cm of new snow. Strong southwest wind. Treeline temperatures around -5 C. Freezing level 1200 m.

Sunday: 5-10 cm overnight then clearing. Light southwest wind. Treeline temperatures around -8 C. Freezing level valley bottom.

Monday: Flurries with sunny periods. Light southeast wind. Treeline temperatures around -8 C. Freezing level valley bottom.

Avalanche Summary

Reports from Wednesday and Thursday indicate increasing slab reactivity prior to burial by the current storm. There were several reports of natural size 2 avalanches in alpine terrain as well as several human triggered size 1 wind slabs around treeline. The most reactive slabs were on convex wind-affected slopes. Most avalanches were in the top 20-30 cm of snow.

Avalanche activity is expected to be large and widespread on Saturday.

Snowpack Summary

15-30 cm of new snow falls amid strong wind over 30-60 cm of settling snow from the past week. Beneath this recent snow lies a variety of suspect layers. The most prominent and widespread is a crust that formed during last week's atmospheric river. This crust extends into the alpine (as high as 2200 m), and there is potential for a poor bond to snow sitting above it. We are uncertain about how reactive the recent snow will be as it settles over the upcoming days. The snowpack structure is relatively simple beneath the crust, with treeline snow depths around 150-250 cm.

Terrain and Travel

  • Fresh snow rests on a problematic persistent slab, don't let good riding lure you into complacency.
  • Travel in alpine terrain is not recommended.
  • The trees are not the safe-haven they normally are at this time. Terrain at treeline is primed for human triggered avalanches.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.

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.