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Avalanche Forecast

Archived

Mar 12th, 2020–Mar 13th, 2020

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Jasper.

Fresh powder in the trees and out of the arctic wind may be the best option for the next few days.

Weather Forecast

The arctic air is approaching with an expected 5-10cm of snow overnight in the Icefields area, lesser amount to the north. The winds will switch to the E with this new air mass providing some reverse loading on westerly facing slopes. More detailed forecast at: Mountain weather forecast

Snowpack Summary

The Icefields area has a well bridged midpack overlying basal facets and depth hoar. The northern region is weaker with less bridging midpack above the basal facets and depth hoar.The fridge air will make for weak bonding of the new snowfall.

Sun crusts are largely absent and the melt is evident in the valley bottom with rocks starting to appear.

Avalanche Summary

On Wednesday a field team at the Columbia Icefields noted two Deep persistent avalanches up to size 3.5 on SW & NE aspects in the alpine. Cornices loom large and threatening over enticing terrain below but may also be the trigger for the deep persistent weakness. Spindrift and point releases avalanches have also been observed in the past week.

Confidence

The weather pattern is stable 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.

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.