Area closures in Jasper National Park for caribou in winter. No backcountry access in the Tonquin, Brazeau, and north boundary regions of the park. For details follow the “Seasonal closures” link in the Resources below (bottom of page).
This is the primary concern at all elevations. The new snow has settled into a touchy soft slab in many locations. This presents as a windslab in exposed areas, such as cross loaded and lee features at upper elevations.
Point releases have the ability to entrain new snow and accumulate significant mass.
Control work on Wednesday produced several results on this layer, particularly in the alpine where storm slabs were able to entrain enough mass to step down to mid-pack instabilities.
Deep persistent slabs are best managed by:
Cornices are best managed by:
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.
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 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.