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Avalanche Forecast

Archived

Nov 30th, 2021–Dec 1st, 2021

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

Regions

Sea To Sky.

Large, destructive avalanches will occur Tuesday night through Wednesday. Don't mess with avalanche terrain.

Confidence

High -

Weather Forecast

Storm conditions continue.

Tuesday night: 50-80 mm precipitation falling mostly as rain. Freezing level 2500 m. Ridgetop winds in excess of 100 km/h from the southwest.

Wednesday: Wet snow mixed with rain; 30-40 cm. Continued strong to extreme southwest winds. Freezing level lowering slightly to around 2000 m.

Thursday: Cloudy with scattered flurries in the morning, some clearing in the afternoon. Moderate westerly winds. Freezing level dropping to around 700 m with treeline temperatures cooling to around -7 C.

Friday: Dry. Cloudy with some clear spells. Light northeasterly winds. Freezing level around 700 m.

Avalanche Summary

Numerous natural and triggered avalanches, including large storm slabs avalanches (size 3 and 4) sliding on buried surface hoar and deeper buried crusts were reported during the last storm. We expect to see another widespread avalanche cycle during the current atmospheric river, with large, full-path avalanches.

Snowpack Summary

At elevations up to around 2500 m, significant amounts of rain is falling on new snow from earlier in the storm. Until temperatures cool, this will result in a wet, heavy, unstable upper snowpack.

A layer of surface hoar has previously been reported that is buried between 60-100 cm deep. Slightly below this layer is a crust with facets. Surprising large avalanches sliding on these weak layers were reported during the last storm.

Average snow depths at treeline are now likely closer to 150-200 cm; 250+ cm in the alpine. Snowpack depths decrease dramatically below treeline and may still be below threshold for avalanches in some areas. Early season hazards such as rocks, stumps, and creeks are still a concern at these lower elevations.

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • If triggered, storm slabs in-motion may step down to deeper layers and result in very large avalanches.
  • Be aware of the potential for large, deep avalanches to run full path or even longer.

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.