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Avalanche Forecast

Archived

Mar 19th, 2022–Mar 20th, 2022

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

Regions

Northwest Coastal.

An easily triggered buried weak layer has surprised riders with large, deep avalanches recently. A tricky persistent slab problem is best managed through conservative terrain selection.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Unsettled weather continues with light snowfall. Heavier snowfall is forecast for the immediate coast and further up some inlets, but it is looking unlikely that it will push very far inland.

Saturday night: Flurries around 5 cm. Moderate southwest ridgetop wind. Alpine high around -8 °C. Freezing level valley bottom.

Sunday: Snowfall 2-10 cm of snow expected. Moderate to strong south wind. Alpine high around -5 °C. Freezing level rising to 800 m through the day. 

Monday: Snowfall 10-20 cm. Strong southwest wind. Alpine high around -1 °C. Freezing level rising to 1500 m through the day. 

Tuesday: Snowfall 20-40 cm. Strong south wind. Alpine high around -1 °C. Freezing level dropping to 1000 m through the day. 

Avalanche Summary

On Thursday and Friday, northwest of Terrace, large to very large avalanches were being triggered by riders and vehicles. These avalanches:

  • had crowns 60-100 cm deep.
  • were failing on a layer of fairly large (10 mm), weak, feathery, surface hoar crystals that were buried early in March.
  • were occurring mostly on northeast facing slopes around treeline.
  • were easily triggered, sometimes remotely and propagating long distances.

Also on Friday, explosive control work near Shames produced large avalanches on an even deeper weak layer, buried in mid February.

Snowpack Summary

40-80cm of recent snow has fallen, with strong southwest winds creating deeper deposits in lee terrain features. Low elevations may hold 10-30 cm of wet/moist snow sitting over a widespread crust on all aspects below 1200 m.

50-100 cm below the snow surface, a weak layer of feathery surface hoar crystals could be preserved in sheltered terrain at and above treeline. This weak layer has started producing large avalanches, mostly north and west of Terrace, where moderate to heavy snowfall and wind have continued through the week. In areas further inland, where the storm tapered off earlier, this layer may not be at its tipping point, but I'd still be suspicious of it through the weekend. 

A thick rain crust from mid-February is buried 100-150 cm. The snowpack below is well consolidated.

Terrain and Travel

  • Uncertainty is best managed through conservative terrain choices at this time.
  • Be aware of the potential for remote triggering and large, deep avalanches due to the presence of buried surface hoar.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.
  • Caution around convexities or sharp changes in terrain.
  • Be careful as you transition into wind affected terrain.

Problems

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.

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.