Although the likelihood of triggering avalanches decreases below treeline, alpine terrain is in high hazard and may run to lower elevations. Be cautious with terrain selection and avoid exposure to overhead hazard.
Weather Forecast
Light scattered precipitation and a gradual warming trend on Friday. Heavier snowfall is expected to start Friday night and continue through Saturday with total amounts in the 10-30cm range. Winds will increase from the SW during this storm and freezing levels will creep up to 1400m.
Snowpack Summary
40cm of recent storm snow has been pushed around by intermittently moderate to strong SW winds and created fresh windslabs in exposed areas, particularly in the alpine. In sheltered areas, this new snow sits as a touchy storm slab in many locations. Midpack persistent weak layers (Jan 16, Jan 7, and Dec 15) are still a concern but remain stubborn.
Avalanche Summary
Avalanche control along the Icefields Parkway produced numerous size 3 avalanches in the alpine, and many size 2-2.5 storm slab and loose avalanches at all elevations. Persistent slab avalanches were produced in the alpine where wind loaded areas provided enough of a trigger to step down to these layers.
Confidence
Intensity of incoming weather systems is uncertain on Saturday
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.
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.
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.