New windslabs are expected to be building overnight on Friday. Use caution moving into upper elevations.
Weather Forecast
A warm and wet airmass is colliding into a cold dry airmass along the continental divide. This is expected to produce significant snowfall, amounts for the Jasper forecast region is expected to be 10-30cm overnight on Friday. After this precipitation pulse, there will be a cooling trend and calm winds with minimal precipitation.
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 on Wednesday 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
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.
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.