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Avalanche Forecast

Archived

Mar 5th, 2021–Mar 6th, 2021

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

Regions

Vancouver Island.

Thursday afternoon avalanche control teams at Mount Washington report at 1500 metes on North aspect, ski cutting touchy fresh wind slab up to 50cm in depth, size 1. Reports of numerous skier accidental avalanches with no back ground information have been submitted. Overall touchy avalanche conditions exist as rapidly loading new snow is and will continue to build touchy storm and wind slab.

Past Weather

Thursday night into Friday morning up to 30 centimeters of new snow fell above 1000-1200 m below this elevation precipitation was in the form of rain. Winds where strong, exceeding 60km/hr out of the South East.

Weather Forecast

A series of Pacific storm fronts in the region are forecast to continue to bring to the area heavy snowfall amounts and strong South East wind. Expect freezing levels fluctuation as both cold and warm fronts pass the area and precipitation will fall as predominantly snow, but in zones south of Arrowsmith, intermittent rain is more likely to occur, all dependent on freezing levels and timing. Friday: 30 to 60 cm of snow. Winds Strong from the Southeast, Freezing levels 1200 meters high descending to 700 meters.Saturday: 15 to 20cm of snow, Winds Moderate to Strong from the South East , Freezing level 900 meter high descending to 600 meters.Sunday: 5 to 15cm. Winds Moderate from the South East, Freezing levels 600 to 700 meters.

Terrain Advice

**Avoidance of avalanche terrain during periods of high avalanche hazard is recommended.** Very careful route finding, seeking non avalanche terrain is crucial as a period of high instability and hazard will be in full effect.

Snowpack Summary

New snowfall delivered with strong winds overlies a well developed surface crust on south aspects and a variety of surfaces on north aspects. In many places the new snow is bonding poorly to old surfaces. New Wind slabs have been forming rapidly beginning Thursday afternoon on North aspects with depths reaching 50 cm's.The newly developing instability will continue to grow in depth and destructive size, patience and time is needed for this new instability to settle out. The mid and lower snowpack is well settle and dense. Snowpack heights throughout the island forecast area range from 300 to 500 centimeters.

Snowpack Details

  • Surface: New snow and wind affected snow deposited on north aspects, soured and pressed areas on south aspects.
  • Upper: South aspects a crsut exisits that and on north aspects old windslabs and some preseved snow can be found.
  • Mid: Old unreactive crusts, overall dense and well settled.
  • Lower: Well settled and dense.

Confidence

High - Certainty with weather forecasts models for heavy precipitation amounts and wind provides a strong mental model of expected snowpack conditions and avalanche hazard and problems for the coming forecast period.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.

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.