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Avalanche Forecast

Archived

Nov 9th, 2014–Nov 10th, 2014

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

Regions

Kananaskis.

Early season avalanche hazard exists at higher elevations in isolated terrain features. Be mindful of terrain above you. Consider the consequences of even a small avalanche when in steep/exposed terrain and avoid terrain traps.

Confidence

Poor

Weather Forecast

Snowfall should end overnight Sunday. Monday will see light to moderate northerly winds and very cold temperatures with the mercury bottoming out near -27 degrees.

Avalanche Summary

Nothing new observed, but visibility was poor.

Snowpack Summary

Up to 20cm of new snow at treeline in past 36hrs with increasingly strong NE winds. November rain crust buried 5 to 10cm at treeline. Early season observations are very limited.

Problems

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.

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.