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Avalanche Forecast

Archived

Feb 8th, 2021–Feb 9th, 2021

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 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, human triggered possible.

Regions

South Columbia.

Triggering large avalanches remains likely in wind-drifted snow or on open glades near treeline where a buried weak layer persists. Persistent slab avalanches can travel far and can be difficult to predict, so a conservative approach is recommended. 

Confidence

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

Weather Forecast

Brrrrrr! Cold and dry conditions persist under arctic air

Monday night: Mostly clear, light northwest wind, alpine temperature -23 C.

Tuesday: Clear, light variable wind, alpine high temperature -18 C. 

Wednesday: Mix of sun and cloud, light northwest wind, alpine high temperature -20 C.

Thursday: Mainly sunny, light northeast wind, alpine high temperature -23 C.

Avalanche Summary

A natural cycle of large (size 2-2.5) wind slab avalanches were reported over the weekend. These avalanches released on north through east through south aspects above 2000 m and broke 30-80 cm deep. A few of these wind slabs were triggered by cornice falls. In this MIN from London Ridge, observers reported a very large wind slab avalanche that may have stepped down to a deeper layer. 

Reports of human-triggered avalanches breaking on the late January surface hoar continue to trickle in. These avalanches have been primary occurred in the near treeline elevation band. However, this MIN report and this MIN report from over the weekend are helpful examples of how cutblocks or "treeline-like" features that are below treeline have caught groups off-guard. This MIN report from last week near Kokanee Pass offers a sobering look at the potential for this problem to propagate widely across features.

Numerous small (size 1-1.5) loose dry avalanches in unconsolidated snow have been reported in steep terrain.

Snowpack Summary

Up to 45 cm of low density snow over the past few days has combined with moderate northwest winds to create wind slabs which may remain reactive in lee features. In sheltered areas, cohesion-less powder may be prone to dry loose avalanches that can run far and fast in these cold, dry conditions. With clear skies, steep slopes in direct sun may rapidly warm midday despite the cold temperatures, and sun crusts may develop.

80-130 cm of snow from the past week is settling over a weak layer of surface hoar that has shown reactivity at treeline or in "treeline-like" features below treeline. This persistent weak layer has potential to surprise backcountry users with how wide the fracture can travel across slopes. This layer will be slow to gain strength and requires careful terrain selection.

A less reactive layer of surface hoar or facets buried in early January can be found down 100-160 cm.

The mid/lower snowpack is generally well settled and strong in most areas.

Terrain and Travel

  • Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

Problems

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.

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.