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Avalanche Forecast

Archived

Mar 31st, 2018–Apr 1st, 2018

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

Regions

Northwest Coastal.

Storm slabs exist in the south of the region from recent snowfall. This overlies a couple touchy weak layers. Be cautious on southerly aspects when the sun is out. Conservative decision-making is recommended.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

SUNDAY: Early-morning snowfall then mostly sunny, accumulation 2 to 5 cm with possible localized higher amounts from convective flurries, light northeasterly winds, alpine temperature -9 C, freezing level 600 m.MONDAY: Mostly cloudy with afternoon snowfall, accumulation 1 to 3 cm, light southerly winds, alpine temperature -9 C, freezing level 600 m.TUESDAY: Mostly cloudy with early-morning snowfall, accumulation 5 to 10 cm, light southwesterly winds, alpine temperature -10 C, freezing level 500 m.

Avalanche Summary

On Friday, a natural cycle within the recent storm snow occurred, failing as storm slabs and loose dry avalanches. They were small to large (size 1 to 2), on all aspects, and at all elevations. See this MIN report to observe some of the avalanches.Previously in the week, large persistent slab avalanches were reported at all elevation bands, on east to northeast aspects. These were failing on the early- and mid-March layers described in the Snowpack Discussion.

Snowpack Summary

Thursday’s storm dumped 30 to 40 cm of snow in the south of the region, such as around Terrace and Shames.  There is now about 70 to 90 cm of storm snow that overlies two layers of surface hoar, which were buried early- and mid-March. At low elevations, the storm snow sits on a melt-freeze crust.Dormant weak layers exist deeper in the snowpack.  Layers of crusts, facets, and isolated surface hoar from mid- and late-February are buried 100 to 150 cm.  Near the bottom of the snowpack, weak and sugary facets exist in shallower parts of the region, such as the far north.

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.

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.