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Avalanche Forecast

Archived

Dec 15th, 2021–Dec 16th, 2021

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

Regions

Cariboos.

A concerning avalanche on Tuesday suggests that a persistent slab problem may be developing in the south of the region. Use extra caution near treeline and assess the local snowpack stability before committing to any serious terrain features. 

Confidence

Low - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast. Uncertainty is due to the speed, direction, or duration of the wind and its effect on the snowpack.

Weather Forecast

A weak upper trough is expected to cross the region on Wednesday night bringing light snowfall to the region. The Arctic high pressure continues to influence the region on Thursday and Friday before a relative weak storm system reaches the region on Saturday. 

Wednesday Overnight: Light snowfall 2-6 cm, moderate SW winds, treeline temperature around -14 °C.

Thursday: Lingering flurries in the morning 1-3 cm, clearing skies in the afternoon, moderate to strong winds shifting to a NW direction, treeline high around -14 °C.

Friday: A mix of sun and cloud, moderate to strong W-NW winds, treeline high around -16 °C. 

Saturday: Light snowfall, moderate to strong S-SW winds, treeline high around -10 °C. 

Avalanche Summary

On Tuesday, a ski cut triggered a size 2.5 persistent slab near Blue River. This occurred on a treeline feature on a NW aspect at 1800 m and failed on the December 1 crust/facet interface down around 70 cm. This avalanche propagated 150 m wide across multiple sparsely treed features suggesting that the layer has the potential to be highly reactive if triggered. This has been the only recent avalanche on the December 1 layer in the region suggesting it is either an isolated event or that the layer is just starting to wake up and become a problem.

On Thursday, wind slabs are expected to remain a concern in the region with a bit of new snow and potentially strong SW-NW winds. In the south of the region, the December 1 interface is creating a concerning persistent slab problem near treeline. Until more is known about the nature of this persistent slab problem, conservative terrain selection remain critical and recently wind loaded features around treeline should be avoided. 

Snowpack Summary

The region typically saw 15-25 cm of new snow over the weekend with strong SW winds which formed reactive wind slabs in exposed terrain. Another 15-25 cm of new snow accumulated on Monday and Tuesday which generally appears to have accumulated without any substantial wind. A bit of new snow Wednesday overnight plus moderate to strong winds from the SW shifting to the NW on Thursday are expected to form new wind slabs in exposed terrain. 

Two interfaces from early December may be found down around 60-100 cm. The December 1 interface consists of a thick crust with facets and appears to be most prominent in the south of the region. This layer resulted in a human-triggered avalanche on Tuesday with a surprisingly wide propagation. It is unclear whether this layer is only reactive in isolated areas or it may be waking up as more load is being added to the snowpack. Regardless, this layer should be treated with the upmost respect until more information becomes available, especially in the south of the region. The December 7 interface consists of a thin crust and/or surface hoar which seems to be most prominent in the north of the region. This layer now appears to have gone dormant over the past few days but it had been reactive over the past weekend. 

The lower snowpack is now generally well settled and stable although an old, faceted crust is likely found near the base of the snowpack. 

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of a persistent slab.
  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • Be alert to conditions that change with elevation and wind exposure.

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.