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Avalanche Forecast

Archived

Feb 13th, 2013–Feb 14th, 2013

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

Regions

Kananaskis.

Recent snow and extreme NW winds are creating storm slabs that are sensitive to human triggering. This new snow has buried a wide variety of layers that will give inconsistent shear results. Evaluate the snowpack carefully.

Confidence

Fair - Due to limited field observations

Weather Forecast

NW winds will continue on Thursday, and will increase in speed through the day. No precipitation is expected and alpine temperatures will range from -18 to -6 degrees.

Avalanche Summary

Nothing new, but observations were limited.

Snowpack Summary

Up to 12cm of new snow at treeline in the past 24hrs. Storm slab development in alpine and treeline areas with slabs between 20 and 30cm deep. Previously formed hard slabs that are widespread on NW through S aspects are now well hidden under the new snow. Weak and facetted snowpack remains at lower altitudes.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.