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Avalanche Forecast

Archived

Dec 10th, 2016–Dec 11th, 2016

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.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Cariboos.

A few more cm of new snow may continue to develop thin wind slabs.

Confidence

Moderate - Wind speed and direction is uncertain

Weather Forecast

Light snow and moderate westerly winds overnight, expect a couple of cm by morning. Alpine temperatures around -15 on Sunday with moderate northwest winds and broken skies. Clear and cold on Monday with alpine temperatures around -20 and moderate northwest winds. Clear and cold on Tuesday with light north winds.

Avalanche Summary

There are no new reports of avalanche activity. Some sluffing has been reported in steep terrain.

Snowpack Summary

Surface snow has been facetting during this period of cold weather, and last weeks storm snow has been settling slowly. Areas sheltered from the wind may be developing a new surface hoar layer. The mid-november crust is buried down 100-180 cm and produces variable results in snowpack tests. Moderate results may be more likely in shallower snowpack areas, and deeper snowpack areas may be more likely to show no results on this layer. Professionals continue to monitor the crust for facet develop that may provide a weak layer above a hard sliding surface in the future.

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.