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Avalanche Forecast

Archived

Nov 24th, 2016–Nov 25th, 2016

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

Regions

Jasper.

Like lipstick on a Pig, the incoming storm snow will bury early season hazards at lower elevations and build onto the wind slab tree line and above.

Weather Forecast

10-25cm forecasted for the Icefields Parkway Thursday night and into Friday, which will be accompanied by moderate south winds. The weekend will bring scattered flurries, light winds with mainly cloudy skies.

Snowpack Summary

On lee slopes, wind slab sits on top of a 5-10cm thick crust between roughly 2100m and 2600m. These slabs may be touchy in cross-loaded areas within the elevation band where the crust exists. Facets are present on top of the crust and will be the layer to watch with the incoming storm snow.

Avalanche Summary

No new avalanches observed

Confidence

Intensity of incoming weather systems is uncertain on Friday

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.