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Avalanche Forecast

Archived

Feb 22nd, 2020–Feb 23rd, 2020

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

Regions

Cariboos.

Touchy storm slabs are developing over a fragile layer of surface hoar. Human triggered avalanches are likely on Sunday.

Confidence

Moderate - Uncertainty is due to how buried persistent weak layers will react with the forecast incoming weather.

Weather Forecast

SATURDAY NIGHT: Increasing cloudiness, light to moderate south wind, alpine temperature -13 C, freezing level below valley bottom.

SUNDAY: 5-15 cm. snow, moderate south wind, alpine temperature -7 C, freezing level 500 m

MONDAY: Cloudy with possible flurries; 0-3 cm, light southwest wind, alpine temperature -5 C, freezing level 700 m

TUESDAY: Mix of sun and cloud, light southwest wind, alpine temperature -6 C, freezing level 500 m.

Avalanche Summary

Numerous large cornice falls have been reported over the last few days. Many of them have not triggered slabs on the slopes below, but a few have, resulting in very large (size 3) avalanches. A cornice triggered size 3 deep persistent slab avalanche was reported on a steep convexity at treeline on Tuesday. This suggests large avalanches are still possible with large triggers in isolated locations. 

Snowpack Summary

5-15 cm of new snow has buried a widespread layer of surface hoar (size 5-15 mm.). This layer exists on all aspects and elevations except for steep solar aspects where it was melted by sun and windward alpine slopes where the layer was flattened by wind before being buried. Surface hoar sitting on a thin sun crust may exist on lower angle solar aspects which is a particularly nasty combination. The new snow will likely become increasingly reactive as it settles into a cohesive slab. The mid and lower snowpack is generally well settled and strong.

Terrain and Travel

  • Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
  • Avoid open slopes and convex rolls at and below treeline where buried surface hoar may be preserved.
  • Be alert to conditions that change with elevation and wind exposure.
  • Cornice failure may trigger 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.