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Avalanche Forecast

Archived

Nov 24th, 2021–Nov 25th, 2021

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

Regions

Vancouver Island.

Forecast heavy rain will be eroding our snowpack on Thursday as well as promoting loose wet avalanche activity. If freezing levels manage to stay lower than expected, reactive storm slabs will form rapidly at higher elevations.

Confidence

Moderate - Forecast precipitation (either snow or rain) amounts are uncertain.

Weather Forecast

Wednesday night: Cloudy with increasingly wet flurries bringing 10-30 cm of new snow above 1500 metres, rain below. Strong to extreme southwest winds. 

Thursday: Cloudy with another 20-60 mm of rain. 10-30 cm of high alpine snow possible. Strong to extreme southwest winds. Treeline high temperatures around +3 with freezing levels rising to between 2200-2700 metres.

Friday: A mix of sun and cloud. Light to moderate southwest winds. Treeline high temperatures around -2 with freezing levels returning to about 900 metres.

Saturday: Cloudy with heavy rain; 20-60 mm. Strong to extreme southwest winds. Treeline high temperatures around +5 as freezing levels jump to 3000 metres.

Avalanche Summary

No avalanches have been reported in the region. Forecast heavy rain through Thursday will promote widespread wet loose avalanche activity while unfortunately eroding a lot of our snowpack. Precipitation and warming appear to be tightly linked through Thursdays' event, meaning significant accumulations of new snow are not expected. If freezing levels end up staying lower than expected, reactive new storm slabs could form in the alpine.

Snowpack Summary

Thursday's storm will bring 40-60 mm of precipitation to the region, however much of this will fall as rain. Areas directly adjacent to the west coast of the island might see almost double this amount. As temperatures cool into the end of the day Thursday we could see around 10-20 cm of new snow accumulate over the rain-wetted surface. 

These final accumulations of dry snow should bond quite rapidly to the underlying wet grains, however it's expected that small, reactive wind slabs will form in specific wind-loaded features in the lee of ridgecrests and other exposed terrain features in the alpine.

Preliminary investigations into the region's existing snowpack suggest the snowline has reached about 850 metres, but that snowpack depths remain below threshold for avalanches below about 1300 metres and in the entire below treeline elevation band. Alpine snowpack depths are likely approaching 150 or more cm, with that depth tapering dramatically with elevation to about 30-60 cm at treeline.

Terrain and Travel

  • As surface loses cohesion due to melting, loose wet avalanches become common in steeper terrain.
  • Keep in mind that wet avalanches can be destructive due to their high density.
  • Be alert to conditions that change with elevation.

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.