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Avalanche Forecast

Archived

Jan 12th, 2020–Jan 13th, 2020

Alpine
Natural avalanches unlikely, human triggered possible.
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 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.

Regions

Cariboos.

A buried weak layer has potential to produce large avalanches around treeline elevations, warranting extra caution around steep open slopes.

Confidence

Moderate - Uncertainty is due to how quickly the snowpack will recover and gain strength.

Weather Forecast

SUNDAY NIGHT: Clearing overnight, light wind from the north, alpine temperatures drop to -35 C.

MONDAY: Mostly sunny, light wind from the north, alpine high temperatures around -25 C.

TUESDAY: Sunny, light wind from the north, alpine high temperatures around -28 C.

WEDNESDAY: Sunny, light wind from the north, alpine high temperatures around -28 C.

Avalanche Summary

There have been limited field observation recently, but enough to suggest the persistent slab avalanche problem remains a serious concern. A large persistent slab avalanche was triggered by a rider in the neighbouring Clemina area on Friday in upper treeline terrain (see the MIN report) and riders on Belle Mountain near McBride reported "thunderous" whumpfing in south facing terrain at treeline. Over the past week there have been several reports of avalanches releasing on this problematic surface hoar layer (check out this MIN, this MIN, and this MIN for helpful illustrations). Looking forward, this problem appears to have variable distribution across the region, meaning steep terrain should continue to be approached cautiously.

Snowpack Summary

Low density snow continues to accumulate. Most areas likely have 10-30 cm of soft snow, but stiffer and reactive slabs could be forming in terrain affected by the wind. Recent storms have loaded a concerning layer of surface hoar from late December, which is now buried 60-120 cm deep. Recent observations and snowpack tests suggest the reactivity of this layer is now variable across the region. Preserved surface hoar could potentially be found on sheltered slopes anywhere in the region, with the potential for producing large avalanches.

Terrain and Travel

  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Choose slopes that are well supported and have limited consequence.

Problems

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.

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.