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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 and human triggered avalanches likely.
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.

Regions

South Coast.

Heavy rain and wind will create dangerous avalanche conditions. Wait out this storm as 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.

Weather Forecast

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

MONDAY NIGHT: 30-45cm overnight with strong southwest winds. Freezing levels rise to 2000m with precipitation falling as rain below. 

TUESDAY: 10-15cm above freezing level at 1800m. Strong southwest winds. 

Overnight, 20-40mm of rain with freezing levels peaking at 2500m.

WEDNESDAY: Heavy rain continues with 50-90mm and freezing levels around 2200m. Strong southwest winds. 

THURSDAY: The front exits leaving clearing skies and no precipitation expected. Freezing levels rise to 2500m over the day, with light easterly winds. 

Avalanche Summary

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

Small loose wet avalanches in the new snow and above the melt-freeze crust were reported on Sunday. Skier triggered wind slabs were reported on Sunday, failing on the recent rain crust on south facing treeline slopes. 

Snowpack Summary

Heavy mixed precipitation and warm temperatures will rapidly create a wet and saturated snow surface with little cohesion. Below around 1200 m, the new snow is overlying a hard melt-freeze crust. Expect this storm to break down any surface crusts and saturate the snow below. 

Around 100 to 150 cm deep, a thin and hard melt-freeze crust may sit above sugary faceted grains that formed during the cold spell in late December. Reports suggest that the snowpack may be bonding well to these previous surfaces.

The middle and base of the snowpack are strong, consisting of well-bonded snow and various hard melt-freeze crusts.

Terrain and Travel

  • The more the snow feels like a slurpy, the more likely loose wet avalanches will become.
  • If triggered loose wet avalanches may step down to deeper layers resulting in larger avalanches.
  • A moist or wet snow surface, pinwheeling and natural avalanches are all indicators of a weakening snowpack.
  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.

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.