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

Feb 8th, 2017–Feb 9th, 2017

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

Regions

Sea To Sky.

Natural and human triggered avalanches are very likely on Thursday. Travel in avalanche terrain is not recommended.

Confidence

High -

Weather Forecast

Wednesday night: 25-30 cm new snow / Strong, southwesterly winds/ Freezing level beginning to rise.Thursday: 30-40 cm new snow / Strong, southwesterly winds / Freezing level rising to 1000-1500 m.(Cooler in the north)Friday: 5-10 cm new snow / Moderate to strong, southwesterly winds / Freezing level 800-1000 m.Saturday: Mostly cloudy / Moderate, southwesterly winds/ Freezing level around 1000 m.

Avalanche Summary

On Tuesday, a size 1.5 wind slab and a 1.5 storm slab were triggered by skiers west of Whistler. Heavy snow, strong winds, and warming is elevating the avalanche danger to HIGH on Thursday.

Snowpack Summary

40-80 cm of recent storm snow has buried a wide variety of old snow surfaces including stiff wind slab or wind effected snow at upper elevations, sun crust on steep southerly slopes, surface hoar(up to 10 mm) in sheltered locations. In sheltered ares where the recent storm snow is overlying surface hoar(weak, feathery crystals), you may see increased reactivity on this layer as the storm snow begins to settle into a more cohesive slab. The mid-January interface (facets) is buried approximately 100-180 cm down. The mid and lower snowpack is generally well settled (strong). However, there remain a number of facet and crust layers that are currently dormant but will require monitoring with additional loading.

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.