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Avalanche Forecast

Archived

Dec 3rd, 2019–Dec 4th, 2019

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, 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.

Regions

Jasper.

Avoid areas where wind loading is present and/or observable during the storm.

Periodic highway closures (up to 1.5 hours) on Highway 93N near the Icefields for Avalanche Control. Check Alberta 511 for details.

Weather Forecast

A Pacific front, laden with moisture will pass over the park bringing snow and strong Westerly winds for the next 24hrs. By midday Wednesday conditions will clear and freezing levels along with the winds will fall rapidly.

Details here: Mountain Weather Forecast.

Snowpack Summary

New snow falling on to a mix of surfaces; surface facets, surface hoar, and previous windslab and/or hard wind pressed surfaces. New building windslabs in exposed areas in the alpine and treeline. Oct. and Nov. crusts preserved in the mid and lower snowpack; both seem have a good bond to the overlaying snow.

Avalanche Summary

No new avalanches observed or reported.

Confidence

Forecast snowfall amounts are uncertain on Wednesday

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.