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Avalanche Forecast

Archived

Jan 1st, 2017–Jan 2nd, 2017

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

Regions

Kootenay Boundary.

Cold north winds have been blowing. Watch for fresh wind slabs, particularly on southerly aspects.

Confidence

High -

Weather Forecast

MONDAY: Dry with clearing skies. Winds northeasterly 20-30 km/h at ridgetop. Ridgetop temperatures around -13C. TUESDAY: Dry and sunny. Winds northeasterly 10-15 km/h. Temperatures around -18C. WEDNESDAY: Dry and sunny. Winds northeasterly 30-50 km/h. Temperatures around -18C.

Avalanche Summary

No avalanches reported in the last 48 hours.

Snowpack Summary

This region saw 30-60 cm new snow during last week's storms. The new snow sits over a weak layer buried on Boxing day that was initially reactive but now appears to have gained strength. Recent winds switched from mainly southwesterly to northerly, "reverse loading" areas that were previously scoured. Slightly lower in the snowpack is an interface buried mid-December, now down 40-100 cm. This layer appears to be well bonded in many parts of the region but was reactive for a while last week west of Trail and Castlegar where preserved surface hoar was thought to be responsible for four small (but surprising) skier trigger avalanches. It will be important to continue to monitor this layer for further signs of reactivity.

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.