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

Regions

South Coast Inland.

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

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather.

Weather Forecast

An intense Pacific front plows through on Saturday and hammers the region with snow and wind

Friday night: Cloudy, 5-15 cm of snow, strong southwest wind, treeline temperatures rising to -4 C overnight, freezing level rising to 1200 m.

Saturday: Cloudy, 5-15 cm of snow, strong southwest wind, treeline temperatures dropping to -8 C, freezing level dropping to valley bottom by end of day.

Sunday: Mainly cloudy, up to 5 cm of snow, moderate southwest wind, treeline temperatures near -10 C, freezing level around 500 m. 

Monday: Mix of sun and cloud, isolated flurries with up to 5 cm of snow, light winds becoming east, treeline temperatures near -8 C, freezing level around 500 m.

Avalanche Summary

 We expect that natural and human triggered avalanches will release large and run far during the storm. 

Snowpack Summary

A potent storm with strong wind is forecast to bring 15-30 cm of new snow to the mountains by the end of Saturday, favoring areas south in the region near Allison Pass. 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 load. Closely monitor how the new snow is bonding to the old surface as the cold snow is not expected to bond well to previous snow surfaces.

In the north of the region, the snowpack near upper treeline elevations is complex and warrants conservative route selection. Weak faceted snow can be found near two possible crust layers that formed in early December, which may become reactive with loading from new snow. Our models suggest that this layer may be most pronounced at elevations between 1400-1800 and in areas north in the region, like the Hurley.  

The south of the region has seen substantially higher snow totals over the past week, with some areas seeing 50+ cm. Expect to find deeper snow accumulations above the December crust and anticipate larger, more reactive storm slab avalanches.

Having endured warmer temperatures and more rainfall, the southern part of the region is just reaching the threshold for avalanches at most elevations. 

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.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.

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.