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Avalanche Forecast

Archived

Jan 11th, 2020–Jan 12th, 2020

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 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.

Regions

Cariboos.

Questions remain about which slopes have the potential to produce large persistent slab avalanches. Cautious route-finding and conservative terrain choices are recommended.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

SATURDAY NIGHT: Mostly cloudy, light to moderate wind from the northwest, alpine temperatures drop to -25 C.

SUNDAY: Mix of sun and cloud with isolated flurries and trace accumulations of snow, light wind from the north, alpine high temperatures around -20 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.

Avalanche Summary

No new avalanches have been reported over the past three days. A large persistent slab avalanche was triggered by a rider in the Clemina area on Friday (see the MIN report). Although this is in the neighboring North Columbia region, a similar problem exists in the Cariboos. Over the past week avalanches releasing on the same surface hoar layer have been reported in the Cariboos. Check out this MIN, this MIN, and this MIN for helpful illustrations of slopes that are likely to harbor this problem. 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.
  • Be especially cautious as you transition into wind affected terrain.
  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.

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.