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

Jan 10th, 2022–Jan 11th, 2022

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

Regions

Sea To Sky.

Heavy rain, snow and wind will rapidly destabilize the snowpack. Sit out this storm, travel in avalanche terrain is not recommended. 

Confidence

High - We are confident the likelihood of avalanche will increase with the arrival of the forecast weather. Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Weather Forecast

A series of fronts moves inland creating warm, wet and windy conditions.

MONDAY NIGHT: 20-40cm with freezing levels rising to 1500m. Strong southwest winds. 

TUESDAY: Light precipitation continues with 10-25cm expected above 1700m and rain below. Strong southwest winds. An additional 15-50cm overnight with freezing levels rising to 1900m. 

WEDNESDAY: Strong and extreme southwest winds. A mix of snow and rain, 15-50 cm expected above the freezing level at 1900m, rain below. 

 

THURSDAY: The front exits leaving clearing skies and no precipitation expected. Freezing levels rise above 2000m, with light easterly winds. 

Avalanche Summary

A widespread natural avalanche cycle is expected at all elevations with the incoming heavy precipitation and warm temperatures.

A natural slab avalanche cycle was observed near Squamish on Sunday. Avalanches were observed to size 3 on all aspects below treeline, and south facing aspects at treeline. 

A size 2.5 naturally triggered slab avalanche was reported near Whistler, thought to have failed on the early December crust/facet combination. Small avalanches may step down to deeply buried weak layers such as this. 

Snowpack Summary

Heavy mixed precipitation and warm temperatures will rapidly create a wet and saturated snow surface with little cohesion. At higher elevations strong winds will load dense snow into wind affected features lee to the strong southwest winds. 

Below 1200 m in parts of the region close to the coast, the last week's rain produced a hard melt-freeze crust. Expect this storm to break down any surface crusts and saturate the snow below. 

This recent precipitation adds to the 100+ cm of snow that has fallen since January 1, which may overly sugary faceted grains that formed during the cold spell in late December.

Around 150 to 250 cm deep, another weak layer of faceted grains may be found above a melt-freeze crust that formed in early December. The layer is most prominent between 1700 and 2100 m. Avalanches on this layer are large, but sporadic and isolated. The most likely place to trigger it would be in thin, rocky snowpack areas. The lower snowpack is well-settled and strong.

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow and wind.
  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • A moist or wet snow surface, pinwheeling and natural avalanches are all indicators of a weakening snowpack.
  • If triggered loose wet avalanches may step down to deeper layers resulting in larger avalanches.

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.