Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Dec 17th, 2016–Dec 18th, 2016

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 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

Cariboos.

Cranking winds and new snow will likely build fresh storm and wind slabs that may be touchy to rider triggers.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain on Sunday

Weather Forecast

A series of Pacific frontal systems will hit the Interior region starting tonight and continue through next week. Each system will be a bit stronger bringing moderate to heavy snow amounts and strong winds. Sunday: Cloudy, alpine temperatures -14 with West winds 40-55 km/h. New snow 10-20 cm.Monday: Snow 15-25 cm with alpine temperatures near -12 and ridgetop winds West 50-70 km/h.Tuesday: A trace of new snow with alpine temperatures -11 and ridgetop winds West 30-45 km/h.

Avalanche Summary

No new avalanche reports from Friday. With forecast strong winds and storm snow, fresh storm slabs may be triggered by light loads (skiers, sledders).

Snowpack Summary

Continued cold temperatures have left us with a variety of snow surfaces including  facets at all elevations and some surface hoar in sheltered locations. Wind slabs exist in lee terrain at treeline and in the alpine. 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 (sugary snow crystals) development that may provide a weak layer above a hard sliding surface in the future.

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.