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Avalanche Forecast

Archived

Feb 8th, 2023–Feb 9th, 2023

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

Regions

Vancouver Island, East Island, North Island, South Island, West Island.

Forecast flurries and any loose snow still available for transport will be going for a ride on an extreme southwest wind on Thursday. Watch for blowing snow and expect rapid slab formation on leeward slopes if you see it happening. Winds this strong can form slabs surprisingly low in the terrain.

Confidence

Moderate

Avalanche Summary

No new avalanches have been reported in the region.

Numerous natural wet loose releases were observed on Monday at treeline and below as rain saturated our recent storm snow. Alpine observations are still lacking, however with precipitation falling as snow, higher elevations likely experienced some degree of natural avalanche cycle during the most recent storm pulse.

Looking forward, the highest elevations of the island where dry snow has accumulated remain a concern for wind slab potential. Cooling temperatures should have by now locked the snowpack in place where precipitation has instead fallen as rain.

Snowpack Summary

15-20 cm of dry snow has so far been observed at treeline, with slightly enhanced amounts expected in the alpine in the wake of 20-50 mm of precipitation falling in the region from Monday through Tuesday, mostly as rain and heavily favouring the south and west of the island.

The new snow overlies moist snow above 1300 m and a new breakable crust below this elevation, both from rain preceding snowfall over the course of the storm. This rain saturated as much as 70 cm that accumulated above 700 m from the previous storm pulse at the end of last week.

These upper snowpack characteristics top a melt-freeze crust that is now likely breaking down where it was thinnest. The crust was previously up to 10 cm thick at lower elevations and tapered to 1 cm thick on shaded or high elevation terrain. A few cm of softer snow recently found immediately below this crust is almost certainly now settled and bonded along with the remainder of the snowpack beneath it.

Weather Summary

Wednesday night

Cloudy with flurries bringing 5-10 cm of new snow. Strong south winds.

Thursday

Cloudy with easing flurries from overnight bringing up to 5 cm of new snow before clearing to a mix of sun and cloud. Strong to extreme south winds. Treeline high temperatures around 0 with freezing levels rising to 1300 m.

Friday

Cloudy with flurries bringing 5-10 cm of new snow, light rain to a possible 1200 m. Strong south winds easing to light northeast. Treeline high temperatures around -1 with freezing levels to 1200 m.

Saturday

Cloudy with flurries bringing about 5 cm of new snow. Strong southwest winds. Treeline high temperatures around -2.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Wind slabs are most reactive during their formation.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Make observations and assess conditions continually as you travel.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.