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Avalanche Forecast

Archived

Jan 10th, 2019–Jan 11th, 2019

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

Regions

Cariboos.

Warming starts on Friday in the Carbioos. Pay attention on sun-affected slopes.

Confidence

Moderate - Freezing levels are uncertain

Weather Forecast

THURSDAY NIGHT: Dry, cooling overnight.FRIDAY: Dry with a mix of sun and cloud. Freezing levels rising to around 2000 m. Alpine temperatures around -2C. Light or moderate southerly winds.SATURDAY: Dry and sunny. Inverted conditions with an above freezing layer between 1600m and 2300m. Light southerly winds.SUNDAY: Dry and sunny. Inverted conditions with an above freezing layer between 1600m and 2300m. Light southwesterly winds.

Avalanche Summary

No recent avalanches have been observed in this region.

Snowpack Summary

Wind slabs are reported as being widespread and reactive at treeline and alpine elevations. Below treeline, recent snow is likely settling and gaining strength.There are a few deeper weaknesses in the snowpack. Professionals are still tracking a layer around 150 to 200 cm deep, composed of sugary faceted grains, feathery surface hoar, and a sun crust. The base of the snowpack may also still be composed of weak faceted grains in parts of the region. The likelihood of triggering these deep weak layers is low and would most likely be triggered by humans in areas where the snowpack is shallow.

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.