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Avalanche Forecast

Archived

Feb 8th, 2023–Feb 9th, 2023

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 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.

Regions

Northwest Coastal, Kitimat, Nass, Rupert, Seven Sisters, Shames, Stewart, Howson, Ningunsaw.

Avoid all avalanche terrain! Another natural avalanche cycle is expected in the region on Thursday.

Confidence

High

Avalanche Summary

Evidence of a widespread natural avalanche cycle was observed throughout the region on Monday and Tuesday, with storm slabs and wind slabs observed to an impressive size 3 (very large). Many slabs started off dry but finished running as wet loose slides at the bottom of their runouts.

A MIN from Monday at Shames gives some great mid-storm observations.

This activity should serve as an indication of what's on tap for this next storm pulse.

Snowpack Summary

Forecast heavy snowfall and strong to extreme winds will take over the upper snowpack again Wednesday night through Thursday, building new storm slabs at all elevations.

The new snow will overshadow the 15-40 cm (diminishing with elevation) that constituted our latest storm snow settling over supportive melt-freeze crust found up to 1800m and on all elevations on steep solar slopes. South to southwesterly winds have been creating wind affected surfaces and wind slabs of varying age and reactivity on an ongoing basis.

Recent and forecast storm snow will form only the uppermost fraction of the impressive 100-150 cm of storm snow from the past week that is collectively settling over a layer of facets, crust, and previous wind-affected surfaces in alpine terrain. This interface remains somewhat in question under the patterns of continuous loading and successive natural avalanche cycles.

The mid and lower snowpack continues to bond and stabilize while a number of buried weak layers are still being tracked by professionals in the region, having produced a few large avalanches in the not-too-distant past.

Weather Summary

Wednesday night

Heavy snowfall beginning with 15-30 cm of new snow by morning. Strong to extreme south winds.

Thursday

Cloudy with continuing heavy snowfall bringing another 20-40 cm of new snow. Strong to extreme south winds, easing over the day. Treeline high temperatures around -2 with freezing levels rising to about 700 m, possibly a bit higher.

Friday

Still mainly cloudy as easing flurries leave a final less-than-5 cm of new snow. Storm totals of around 40-70 cm. Light to moderate southwest winds. Treeline high temperatures around -3 and falling over the day.

Saturday

Cloudy with another round of flurries bringin 5-10 cm of new snow. Strong to extreme southwest winds easing over the day. Treeline high temperatures around -3.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Don't let the desire for deep powder pull you into high consequence terrain.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
  • Avoid exposure to overhead avalanche terrain during periods of heavy loading from new snow, wind or rain.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.