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Avalanche Forecast

Archived

Dec 27th, 2019–Dec 28th, 2019

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

Regions

Northwest Coastal.

New snow amounts will vary throughout the region on Saturday. Danger will be HIGH in areas that receive more than 20 cm of new snow.

Confidence

Moderate - Forecast precipitation (either snow or rain) amounts are uncertain. Uncertainty is due to how buried persistent weak layers will react with the forecast incoming weather.

Weather Forecast

FRIDAY NIGHT: Storm arrives with 5-25 cm of snow by the morning, 80-120 km/h wind from the southwest, freezing level climbing to 1000 m. 

SATURDAY: Snow continues throughout the day with another 10-25 cm of snow above 700 m, 80-100 km/h wind from the southwest, freezing level around 1000 m and alpine high temperatures around -1 C. 

SUNDAY: Scattered flurries with 5-15 cm of snow, 30-40 km/h wind from the south, alpine high temperatures around -1 C.

MONDAY: Next frontal system arrives bringing 20-30 cm of snow by the afternoon, 60-90 km/h wind from the southwest, freezing level around 1000 m.

Avalanche Summary

Natural avalanches are expected in parts of the region that receive more than 20 cm of new snow on Saturday. Human triggering will also be very likely on freshly loaded slopes. There is additional concern about the buried surface hoar layers, as the combination of new snow, wind loading, and warming could increase the likelihood of large persistent slab avalanches on these layers.

Over the past week there have been ongoing reports of size 1-2 wind slab and storm slab avalanches (both natural and explosive triggered), but there are no reports of larger persistent slab avalanches. If Saturday's storm doesn't result in a persistent slab avalanche activity, then Monday and Tuesday's more intense storm likely will.

Snowpack Summary

Saturday's storm will bring 15-50 cm of snow to the region with very strong wind and warming temperatures. Expect fresh and reactive storm slabs and wind slabs to form in certain parts of the region. This could also be the extra load needed to wake up one of two buried layers of surface hoar between 40-100 cm deep. These layers were buried a few weeks ago and have been reactive in snowpack tests. Reports from the Shames area suggest buried surface hoar can be found on all aspects, but is more prevalent on southeast to southwest aspects around 800-1400 m, as well as sheltered alpine areas. The lower snowpack is generally considered strong.

Terrain and Travel

  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.
  • Dial back your terrain choices if you are seeing more than 20 cm of new snow.
  • Fresh snow rests on a problematic persistent slab, don't let good riding lure you into complacency.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.

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.