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 25th, 2019–Dec 26th, 2019

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

Regions

Sea To Sky.

Our snowpack structure remains very concerning to avalanche professionals throughout the region. Obvious feedback (natural avalanches) may be diminishing, but our persistent slab problem remains active. Keep seeking out conservative terrain options.

Confidence

High -

Weather Forecast

Wednesday night: Clear periods. Calm or light southwest winds.

Thursday: Cloudy with light flurries developing late in the day, bringing a trace to 5 cm and continuing overnight. Light to moderate southwest winds increasing over the day and becoming strong at ridgetop. Alpine high temperatures around -8.

Friday: Cloudy with new snow totals of 10-15 cm. Light to moderate southwest winds. Alpine high temperatures around -7.

Saturday: Cloudy with scattered flurries bringing 5-10 cm of new snow, continuing overnight. Light to moderate south winds, becoming strong at ridgetop. Alpine high temperatures around -5.

Avalanche Summary

Reports from Monday and Tuesday showed more observations of the widespread large to very large (size 2-3) natural avalanches that have run recently, along with numerous (but diminishing) new explosives-triggered size 2-3 releases, targeted in the Whistler area.

Many more size 2-3 avalanches were triggered by explosives and by skiers on Saturday and Sunday. 

Many of the avalanches mentioned above failed on the mid-November weak layer described in our Snowpack Summary. Many of the larger examples scoured the lower snowpack away to reveal ground. Some of the avalanches were remotely triggered. See here for some photos of one of them.

Human-triggering of large avalanches remains likely at higher elevations. Very cautious route-finding and conservative decision making is currently required for safe travel in higher elevation avalanche terrain.

Snowpack Summary

Large new surface hoar is beginning to be reported on the snow surface in sheltered areas. Below the surface, the upper snowpack consists of around 70 to 120 cm of snow from the storm at the end of last week. 

All this snow overlies a weak layer of surface hoar as well as a deeper (100-200 cm) weak layer of sugary faceted grains and a hard melt-freeze crust buried in mid-November. This unstable structure has been producing large and destructive avalanches, often with light triggers and even remote (from a distance) triggers over the past several days.

This weak and touchy snowpack is atypical for the region and is expected to persist for some time. Conservative terrain choices along with selective avoidance of high-consequence avalanche terrain will be imperative to manage your risk until the snowpack gains strength.

Terrain and Travel

  • Don't let the desire for deep powder pull you into high consequence terrain.
  • Persistent slabs have potential to pull back to lower angle terrain.
  • Make conservative terrain choices and avoid overhead hazard.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

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.