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Avalanche Forecast

Archived

Apr 3rd, 2022–Apr 4th, 2022

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

Regions

South Coast Inland.

There is substantial uncertainty regarding storm snow totals by Monday afternoon but it is likely enough to create dangerous avalanche conditions. The storm snow is expected to be touchy throughout the region and the deeper snowfall areas may see a natural avalanche cycle.

Confidence

Low - Uncertainty is due to the timing, track, & intensity of the incoming weather system.

Weather Forecast

A storm system is expected to continue to impact the region until Tuesday morning. Heavy snowfall is expected for the immediate coastal regions but there is substantial model variability regarding how much will make it to the inland region.

Sunday Night: Snowfall 10-30 cm, strong SW wind, freezing level low around 1000 m/high around 1500 m. 

Monday: Snowfall 10-30 cm, strong SW wind, freezing level high around 1300 m. 

Tuesday: Mainly cloudy with lingering flurries, moderate W wind, freezing level high around 1400 m.

Wednesday: Mainly sunny, light variable wind, freezing level high around 1800 m.

Avalanche Summary

On Saturday in the north of the region, a skier triggered a size 1 wind slab on a northeast aspect at 2450 m which had an average thickness of 25 cm and slid on a melt-freeze crust. In the Coquihalla area, this MIN report and this MIN report describe small skier-triggered soft slab avalanches which were 5-20 cm thick. This MIN report describes wind loading and shooting cracks in the recent 10-15 cm of storm snow. 

On Friday, a ski cut in the north of the region triggered a size 1 wind slab on a northeast aspect at around 2200 m elevation which was 15-20 cm thick. In the Coquihalla area, two natural cornice releases were reported on northwest aspects and a size 1 solar-triggered loose dry avalanche was observed in the alpine. 

Snowpack Summary

The new storm snow will continue to bury a strong, supportive crust which extends to mountain top on solar aspects and to around 2200 m on northerly aspects. Strong southwest wind will be redistributing the new storm snow in exposed high elevation terrain forming touchy wind slabs and building large cornices. 

The rest of the upper snowpack consists of a number of crust/facet/surface hoar interfaces buried in March that seem to have bonded well during the recent warm weather. 

The middle and lower snowpack are generally strong and well bonded. 

Terrain and Travel

  • Watch for fresh storm slabs building throughout the day.
  • Make conservative terrain choices and avoid overhead hazard.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Extra caution is needed around cornices under the current conditions.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

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.