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Avalanche Forecast

Archived

Dec 9th, 2016–Dec 10th, 2016

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

Regions

Kananaskis.

Warmer temps are coming!! Following the cold snap, expect sluffing in steep terrain.

Confidence

High -

Weather Forecast

Mainly cloudy tomorrow with alpine temps climbing to -11!! Winds will be westerly at 15km/hr. No new snow.

Avalanche Summary

Nothing new, however loose dry avalanches from the last 48hrs are still visible.

Snowpack Summary

Not a lot of change in the snowpack as a whole. We are seeing some surface hoar start to develop. The northern region has 10-15mm, while the southern areas have up to 5mm. The treeline snowpack continues to lose strength due to the cold temps. Limited settlement has kept the Nov 12th crust down 50-70cm at treeline elevations. Luckily the winds have also been light keeping snow transport and slab development minimal. Snow depth at Burstall Pass is 110m.

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.