Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Regions
Jasper.
At these temperatures even a minor injury could have severe consequences, plan your day accordingly.
Weather Forecast
A strong ridge of high pressure dominates the North & Central Rockies until Wednesday, dragging cold air down from Alaska. Tuesday: Sunny with cloudy periods developing in the PM. Low of -23 C and High of -18 C with light winds from the North.A detailed mountain weather forecast is available from Avalanche Canada.
Snowpack Summary
50cm recent storm snow came with strong Northerly winds. This storm snow overloaded the Jan 18 persistent weakness (SH in sheltered areas, crust on exposed solar slopes) in deeper snowpack areas, and the weak and facetted base of the snowpack in shallow areas (deep persistent weakness), resulting in a natural cycle of large avalanche activity.
Avalanche Summary
Avalanche control work Monday, between the Icefields and Saskatchewan crossing, produced several large (size 2-2.5) persistent and deep persistent slab avalanches.A natural cycle of large slab avalanches occurred during the most recent storm.Help forecast - share observations HERE, on the Mountain Information Network!
Confidence
Problems
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
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.