Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Regions
Jasper.
Manage your exposure and keep wary to evidence of localized instability such as cracking, whumphing and, recent avalanche activity.
Weather Forecast
Tuesday will be clouds with sun and isolated flurries, alpine temperature high -11 °C, and West 10-25 km/h winds. Wednesday will be a mix of sun and cloud with isolated flurries, alpine temperature low -20 °C and high -10 °C, Northeast 10-30 km/h winds. A detailed mountain weather forecast is available from Avalanche Canada.
Snowpack Summary
Cold temps have faceted the upper snowpack leaving a weak slab over a instability of surface hoar/facets on a crust down 40cm. The thicker spots have a strong mid-pack and bridges the deep persistent basal weakness of depth hoar. A thinner snow-pack can act as a slab initiating the basal facets and depth hoar in the lower part of the snowpack.
Avalanche Summary
No patrol on Monday and nothing new reported. Saturday's field team in Whistler Creek had good ski conditions and no new avalanches in the zone. Recently numerous dry loose up to sz 1 have come out of steep, planar terrain across the forecast region.
Confidence
Problems
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.