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Avalanche Forecast

Archived

Jan 3rd, 2022–Jan 4th, 2022

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

Regions

Lizard-Flathead.

Newly formed storm slabs are expected to be touchy on Tuesday. The region continues to deal with a tricky persistent slab problem and very large avalanches remain possible. Conservative terrain selection remains critical.

Confidence

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

Weather Forecast

Unsettled conditions are expected on Tuesday in the wake of the storm. Periods of light snow and sunny breaks are both possible. 

Monday night: Snowfall 5-15 cm, moderate to strong SW wind, treeline temperature around -8 °C. 

Tuesday: A chance of sunny breaks in the morning, light snow in the afternoon 3-6 cm, light to moderate SW wind, treeline high around -10 °C. 

Wednesday: A mix of sun and cloud with a chance of flurries in the morning, light to moderate N wind, treeline high around -20 °C. 

Thursday: Periods of light snowfall 2-4 cm, moderate to strong SW wind, treeline high around -14 °C. 

Avalanche Summary

Early reports from Monday include explosive triggered storm slabs up to size 2. Ski cutting was triggering size 1 storm slabs and loose dry avalanches. 

On Sunday, a size 2.5 persistent slab avalanche was triggered on an E aspect at treeline. This MIN post goes into more details and has some great photos showing the nature of the problem and the type of terrain where this problem seems most prevalent. On Friday, a size 2.5 persistent slab avalanche was reported on a north aspect at 2000 m elevation. This failed on the early December weak layer down 100-175 cm. Last week, a few surprisingly deep older crowns were observed between Fernie and Sparwood. These persistent slab avalanches also likely ran on the early December crust. 

On Tuesday, recently formed storm slabs are expected to remain reactive to human triggering. These new slabs sit on a weak interface and may be very reactive, especially in wind loaded terrain. The persistent slab problem remains a serious concern and the weight of the new snow may increase the reactivity of these deeper layers. Smaller storm slab avalanches also have the potential to step down to deeper layers resulting in very large avalanches. 

Snowpack Summary

The new storm snow buried a variable snow surface which is likely weak and includes widespread facets, wind affected surfaces, and/or surface hoar in sheltered areas. The new snowfall may have been accompanied by moderate to strong winds and new storm slabs are expected to be most reactive in wind loaded areas. 

The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 90-200 cm. Activity on this layer has been sporadic, but most recently produced large avalanches on January 2 and December 31. This layer has created a low likelihood, high consequence scenario which is best managed through conservative terrain choices and disciplined backcountry travel techniques.

Terrain and Travel

  • Continue to make conservative terrain choices while the storm snow settles and stabilizes.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.