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

Regions

Sea To Sky.

Heavy snowfall and strong wind are creating very dangerous avalanche conditions. Having the skills to recognize and avoid avalanche terrain will be critical to managing your risk on Saturday. Stick to simple, low-angle slopes with no overhead hazard. 

Confidence

Moderate - We are confident a natural avalanche cycle will begin shortly after the arrival of the incoming weather.

Weather Forecast

A fast-moving storm plows through overnight and hammers the region with snow and wind.

Friday night: Cloudy, 20-40 cm of snow above 1000 m, strong southwest wind, alpine temperatures rising to -5 C, freezing level reaching 1000 m and dropping to 700 m by morning.

Saturday: Cloudy, 5-15 cm of snow, strong southwest wind, alpine temperatures cooling from -6 C to -11 C, freezing level dropping from 1000 m to 500 m.

Sunday: Cloudy, 5-15 cm of snow above 500 m, light southwest wind, alpine temperatures near -12 C. 

Monday: Cloudy with sunny breaks, 5-15 cm of snow, light winds becoming east, alpine temperatures near -9 C, freezing level near 600 m.

Avalanche Summary

We expect that natural and human triggered avalanches will release large and run far on Saturday. Cornices could reach their breaking point and trigger large avalanches on slopes below.

Snowpack Summary

A powerful storm with strong wind is forecast to bring 30-60 cm of new snow to the mountains by the end of Saturday. This will create a widespread, reactive storm slab problem that will be particularly pronounced where the snow is drifted by southwest winds. The snowpack will need time to adjust to this rapid, hefty load. Closely monitor how the new snow is bonding, as the cold snow is not expected to bond well to previous snow surfaces. Cornices are large and looming and could reach their breaking point.

The snowpack around treeline is complex and warrants conservative route selection. Weak faceted snow can be found near two possible crust layers that formed in early December. This crust-facet combination may become reactive with rapid loading. Our models suggest that this persistent slab problem may be most pronounced at elevations between 1400-1800. Any steep opening in the trees should be treated as suspect right now.

Average snow depths vary drastically with elevation, with 320-400+ cm in the alpine, 120-200 cm at treeline, and a drastic drop to below the threshold for avalanches below treeline. With this storm event, a greater number of areas at or below treeline elevations may meet the threshold for avalanches. 

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
  • Expect slab conditions to change drastically as you move into wind exposed terrain.
  • Stick to simple terrain features and be certain your location isn't threatened by overhead hazard.
  • Cornice failures could trigger very large and destructive avalanches.
  • The trees are not the safe-haven they normally are at this time. Terrain at treeline is primed for human triggered avalanches.

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.