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Avalanche Forecast

Archived

Jan 13th, 2021–Jan 14th, 2021

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

Regions

South Columbia.

Ease into terrain cautiously on Thursday. Start small and tune in to signs of instability like shooting cracks and recent avalanches. Be mindful that sunshine can have a powerful effect on stability - and on your desire to push into aggressive terrain. 

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

Wednesday night: Easing flurries bringing a final trace to 5 cm of new snow. Light to moderate northwest winds.

Thursday: Mainly sunny. Light variable winds. Alpine high temperatures around -8.

Friday: Cloudy with scattered flurries bringing up to 5 cm of new snow. Light south winds shifting west. Alpine high temperatures around -7.

Saturday: Mainly cloudy. Light variable winds. Alpine high temperatures around -7.

Avalanche Summary

A few preliminary observations from the aftermath of Tuesday's storm validated expectations of a busy day for natural avalanches. One natural size 2.5 (large) storm slab was observed in a lower elevation cutblock that had been crossloaded by strong winds. 

In the Trans-Canada corridor, a size 4 (VERY LARGE) avalanche ran on Mt. Laurie. A few other size 1 and size 2 releases, both natural and skier triggered, were observed in the Galena Pass and Meadow creek areas. Observations were limited in some cases by strong winds.

Looking forward, expect Thursday to be another tricky day to be in the mountains, with new and reactive wind slabs formed in wind-exposed areas and even more widespread storm slabs primed for human triggering in more sheltered areas.

Snowpack Summary

30-40 cm of new snow fell during Tuesday's storm. The new snow buried wind affected surfaces at upper elevations, as well as surface hoar in wind sheltered areas and a thin crust on solar aspects. 

The new snow will take time to form a bond with these previous surfaces, particularly in spots harbouring surface hoar or crust. In exposed areas, elevated winds are almost certainly redistributing new snow into reactive wind slabs and adding to cornices. 

A couple of persistent weak layers exist in the upper to mid snowpack:

  • The upper layer, now found an estimated 70-120 cm deep, is a spotty layer of surface hoar at treeline and below. 
  • The lower layer, now likely closer to 120-190 cm deep, is widespread and may present as decomposing surface hoar and/or a crust.

Avalanche activity on these layers has been dwindling since last week and snowpack tests results have generally indicated the weak layers are gaining strength. Given their age (particularly the deeper layer) and the testing load brought by Tuesday's storm, the outlook is good for these layers to finally become dormant as our current surface instabilities diminish.

Terrain and Travel

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid exposure to steep sun exposed slopes.

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.