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Avalanche Forecast

Archived

Feb 10th, 2021–Feb 11th, 2021

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

Regions

Lizard-Flathead.

Yup, still cold. A conservative trip plan is a good idea when dealing with a persistent avalanche problem and extreme cold weather. 

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

WEDNESDAY NIGHT - Partly cloudy / light north east wind / alpine low temperature near -30

THURSDAY - Cold and clear / light to moderate north east wind / alpine high temperature near -24

FRIDAY - Cold and sunny / light north east wind / alpine high temperature near -20

SATURDAY - Increasing cloud / light to moderate northeast wind / alpine high temperature near -20

Avalanche Summary

On Tuesday there were a couple of new skier triggered avalanches, including a remote triggered size 2 on Mt. Fernie (suspected surface hoar). Also on Tuesday, explosive control yielded wind slab avalanche results up to size 2.

On Monday, skiers accidentally triggered 2 small (size 1) avalanches down 45 cm, likely on surface hoar.

On Sunday a cornice failure triggered a small (size 1) avalanche with a 50 cm crown. Skiers reported sudden results in test profiles on prominent surface hoar on a variety of aspects buried 50 cm deep.

Last week was busy for avalanche activity, on Wednesday (Feb 3) persistent slab avalanche activity really picked up with reports of natural, human, and explosives triggered storm and/or persistent slab avalanches up to size 2 everyday through Saturday (Feb 6). 

On Saturday (Feb 6) riders continued to trigger slab avalanches 20-60 cm deep, documented in a handful of MIN reports (Trespass, Mammoth, Spicy, Different Day). Explosives triggered several large (2-2.5) persistent slab avalanches on northerly aspects below 2000 m.

On Friday (Feb 5), there were numerous reports of natural and human triggered persistent slab avalanches up to size 2.5. Some of these were triggered remotely, as outlined in a MIN report that can be viewed here. There were also numerous natural and explosives triggered dry loose, and storm slab avalanches reported up to size 2. 

Many thanks for all of the great MIN reports over the past week!

Snowpack Summary

Surface faceting and surface hoar growth is occurring with clear nights and frigid temperatures. Recent northerly and shifting winds have reverse loaded features, slabs may be found in lee terrain on a variety of aspects. 

A persistent weak layer lurks 30-70 cm below the surface, consisting of surface hoar, facets, and a crust buried in late January. This layer has been responsible for the majority of recent avalanche reports and has been easily found on all aspects, reports suggest it is touchiest on northerly and easterly aspects.

Below 1600 m a hard melt-freeze crust is underneath 20-40 cm recent snow. A solid mid-pack sits above a deeply buried crust and facet layers near the bottom of the snowpack (150-200 cm deep), which is currently unreactive. 

Terrain and Travel

  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Be aware of highly variable recent wind loading patterns.
  • Avoid terrain traps such as gullies and cliffs where the consequence of any avalanche could be serious.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.

Problems

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.

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.