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Avalanche Forecast

Archived

Jan 18th, 2019–Jan 19th, 2019

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 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.

Regions

South Columbia.

Storm slabs are building above a touchy weak layer. Be extra cautious around steep rolls and wind loaded slopes.

Confidence

Moderate - Forecast snowfall amounts are uncertain

Weather Forecast

FRIDAY NIGHT: 5-15 cm of snow, strong southwest wind, alpine temperatures drop to -8 C.SATURDAY: Flurries easing throughout the day with another 5 cm of snow, strong southwest wind, freezing level climbing to 1300 m, alpine high temperatures around -3 C.SUNDAY: Light flurries in the morning then clearing in the afternoon, moderate north wind, freezing level climbing to 1000 m, alpine high temperatures around -5 C.MONDAY: Mix of sun and cloud, light northwest wind, alpine high temperatures around -8 C.

Avalanche Summary

Slab avalanches will become more likely as snow accumulates above the freshly buried weak layer. The key is watching for signs of this new slab becoming reactive, such as cracking, whumpfing, or stiffer deeper pockets of snow.On Thursday, when there was only about 10 cm of new snow, skiers triggered fast moving sluffs (loose dry avalanches) and small wind slab avalanches on north and east facing slopes. A skier also remotely triggered a size 2 wind slab (60 cm deep) on a southwest alpine slope.

Snowpack Summary

By Saturday, 15-30 cm of snow will have buried a layer of large surface hoar crystals and sun crusts. This will create the potential for fast moving sluffs and thin slab avalanches with wide propagations. The most suspect terrain features are steep slopes and rolls below 2000 m (where the largest surface hoar exists) and steep south-facing slopes in the alpine (where sun crusts exist).The middle and lower portions of the snowpack are generally well-settled and strong. Professionals are tracking a layer around 130 to 180 cm deep, composed of weak faceted grains, surface hoar, and a sun crust. The chance of triggering this layer is low. In shallow snowpack areas, the base of the snowpack may also still be composed of weak faceted grains.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.