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Avalanche Forecast

Archived

Dec 29th, 2019–Dec 30th, 2019

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

Regions

Northwest Coastal.

Avalanche danger will escalate throughout the day as heavy snowfall and warming temperatures weaken the snowpack.

Confidence

Moderate - Uncertainty is due to the timing of the incoming weather system. Uncertainty is due to rapidly fluctuating freezing levels.

Weather Forecast

SUNDAY NIGHT: Light flurries start overnight as strong frontal system arrives, wind increasing from moderate to strong from the southwest, alpine temperatures around -2 C.

MONDAY: Frontal system intensifies throughout the day with 15-40 cm of snow by the afternoon as snow level rises from 600 to 1000 m, strong to extreme wind form the southwest, alpine temperatures reach 0 C.

TUESDAY: Storm continues Monday night with another 20-30 mm of precipitation with rain up to 1200 m by the morning then cloudy in the afternoon, moderate wind from the southwest, freezing level around 1300 m.

WEDNESDAY: Scattered flurries with 5-15 cm of snow, light wind with moderate gusts from the west, freezing level drops to 500 m with alpine high temperatures around -2 C.

Avalanche Summary

The incoming storm will result in natural avalanche activity. Since the storm is expected to hit peak intensity on Monday evening, the most dangerous conditions will be late afternoon and into the evening. The transition from snow to rain could cause a mix of avalanche problems later in the day including storm slabs, wind slabs, and wet loose avalanches on buried surface hoar layers.

Saturday's storm also resulted in natural avalanche activity, with numerous size 2 storm slab avalanches and several size 3 avalanches (on north and east aspects) that potentially ran on the buried surface hoar layers described in the persistent slab avalanche problem. The combination of new snow and warm temperatures on Monday and Tuesday will increase the likelihood of persistent slab avalanches.

Snowpack Summary

The incoming storm will start cold delivering 15-40 cm of new snow by Monday afternoon before it starts raining up to 1200 m on Monday night. The new snow will add to the 15-50 cm of snow that fell Saturday, resulting in the potential for thick storm slab avalanches. Strong wind from the southwest will form formed extra thick unstable slabs in lee terrain. This could be the extra load needed to wake up either of the two layers of surface hoar buried 50-120 cm deep. 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.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Avoid the runout zones of avalanche paths. Avalanches could run full path.
  • Storm slab size and sensitivity to triggering will likely increase through the day.
  • Only the most simple non-avalanche terrain free of overhead hazard is appropriate at this time.

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.