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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

Purcells.

Ease into terrain cautiously on Thursday. Start small and tune in to signs of instability like shooting cracks and recent avalanches. Bear in mind 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: Diminishing cloud with isolated flurries. Moderate to strong northwest winds.

Thursday: Mainly sunny. Light to moderate northwest winds. Alpine high temperatures around -8.

Friday: A mix of sun and cloud. Light to moderate southwest wind shifting northwest. Alpine high temperatures around -7.

Saturday: A mix of sun and cloud. Light west winds. Alpine high temperatures around -7.

Avalanche Summary

Preliminary observations from the Golden area on Wednesday showed explosives control yielding size 2 (large) storm slabs about 40 cm deep, but with a variability in depth that shows good evidence of wind redistribution. Further observations are expected to validate expectations of a busy day for avalanches in the region.

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

15-40 cm of new snow fell in the region during Tuesday's storm. It 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, found 40-60 cm down, is a spotty layer of surface hoar at treeline and below. 
  • The lower layer, found 90-140 cm down, is widespread and can present as surface hoar and/or a crust.

Avalanche activity on these layers has dwindled since last week and snowpack tests results have generally indicated the weak layers are slowly gaining strength. Avalanche activity resulting from the storm may shed some light on whether or not they remain a concern.

The lower snowpack is characterized by more crusts, the most notable is a rain crust from early November that is near the base of the snowpack, surrounded by a weak layer of sugary facets. It is most likely to be reactive to human triggers in steep, shallow, rocky areas with a thin to thick snowpack.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
  • 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.