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Avalanche Forecast

Archived

Dec 4th, 2013–Dec 5th, 2013

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

Regions

South Columbia.

Confidence

Fair - Due to the number of field observations

Weather Forecast

A strong Arctic air mass will continue to dominate conditions in the southern interior. Thursday: Mostly sunny, light NE alpine winds, alpine temperatures around -20CFriday/Saturday: Mostly sunny, light NE alpine winds possibly increasing on Saturday, alpine temperatures as low as -30C

Avalanche Summary

Several natural avalanches to size 2.5 were recently reported across the forecast region on all aspects.  These avalanches primarily consist of the previous storm snow or redistributed wind slabs sliding on the late-November crust/surface hoar interface. 

Snowpack Summary

Snowpack depths are typically 100-140 cm at treeline elevation. The previous storm snow (~30-60cm) overlies the late-November interface which typically consists of sun crusts on steep south facing slopes and surface hoar in sheltered areas. These weak layers are expected to be persistent and will continue to create avalanche problems in areas with enough overlying snow. The current cold temperatures will contribute to the persistence of this weak layer.  Strong NE winds after the storm have caused reverse loading and wind slab formation on SE through W aspects in wind exposed areas.  There are two layers of concern within the mid/lower snowpack but these have recently become inactive: the early November surface hoar is roughly 60cm above the ground and the October rain crust is at the base of the snowpack. While these layers have recently become inactive, residual risk of large, destructive avalanches exists, especially in areas with a thinner snowpack. The October crust can be found in the alpine on north aspects and the early November surface hoar appears to be isolated and drainage specific.

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.

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.