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Avalanche Forecast

Archived

Jan 3rd, 2020–Jan 4th, 2020

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

Regions

Cariboos.

The snowpack will take time to adjust to the load from recent snowfalls. In the meantime continue to choose conservative terrain.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Friday Night: Flurries, accumulation 5-15 cm. Alpine temperature -4 C. Moderate to strong southwest wind. Freezing level 1500 m.

Saturday: Flurries, accumulation 5-10 cm. Alpine temperature -6 C. Moderate west wind. Freezing level 1000 m.

Sunday: Flurries. Alpine temperature -10 C. Moderate west wind.

Monday: Mainly cloudy with scattered flurries. Alpine temperature -11. Moderate southwest wind.

Avalanche Summary

On Wednesday there was a report of a remotely triggered size 2 wind slab avalanche in the alpine. On Wednesday and Thursday there were reports of numerous naturally triggered storm slab avalanches to size 2.5 and 3 on all aspects at all elevations.

Snowpack Summary

40-70 cm of new snow fell through the last week. All this recent snow has buried a layer of surface hoar found at all elevations. In some places the surface hoar may be combined with sun crust on steep sun-exposed aspects.

A weak layer that was buried December 26 is now approximately 50-80 cm deep and may present as surface hoar in sheltered areas, sun crust on steep solar aspects and/or a melt freeze crust below 1700 m.

An additional layer of surface hoar buried mid December is 90-160 cm deep. Avalanche activity on this layer has tapered off, but there is still concern for heavy loads to step down to this layer. A crust from late November is now over 160 cm deep. Concern for this layer is limited to rocky or variable snowpack depth areas in the alpine where it most likely exists as a combination of facets and crust.

Terrain and Travel

  • Be alert to conditions that change with elevation and wind exposure.
  • Avoid freshly wind loaded terrain features.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Be aware of the potential for large avalanches due to the presence of a persistent slab.

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.