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Avalanche Forecast

Archived

Jan 8th, 2017–Jan 9th, 2017

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, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

North Columbia.

Wind is driving the avalanche danger on Monday. I would expect to find touchy wind slabs on lee features below ridgetops and good skiing in sheltered terrain.

Confidence

Moderate - Forecast snowfall amounts are uncertain

Weather Forecast

MONDAY: Snow beginning Sunday evening and is expected to accumulate to 10-20 cm by Monday afternoon. Moderate southwesterly ridgetop winds, and temperatures around -12.TUESDAY: Mix of sun and cloud, moderate northwesterly ridgetop winds, and temperatures around -18.WEDNESDAY: Mostly sunny with cloudy periods, light northwesterly ridgetop winds, and temperatures around -20.

Avalanche Summary

On Saturday, numerous size 1 human triggered wind slabs were reported on northerly aspects. I expect human triggered wind slab activity to increase on Monday with the forecast new snow and wind.

Snowpack Summary

Forecast 10-20 cm of new snow by Monday afternoon and moderate southwest winds are expected to create fresh wind slabs on lee features at treeline and above. Recent snow has also covered old, thicker wind and hard slabs from previous wind events. Persistent weak layers in the mid-pack are giving variable results in snowpack tests, but are generally most touchy in shallow snowpack areas. Recent snowpack tests gave moderate to hard but resistant results on two different layers of facets and/or buried surface hoar in the top metre. The lower snowpack seems to be well bonded, but features a crust/facet deep persistent weakness near the ground, which remains a concern in shallow rocky snowpack areas.

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.