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Avalanche Forecast

Archived

Feb 23rd, 2020–Feb 24th, 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

South Columbia.

The developing storm slabs are expected to be reactive to human triggers on Monday. Careful terrain selection and route finding will be required to effectively manage risk.

Confidence

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

Weather Forecast

SUNDAY NIGHT: Cloudy with flurries; 3-5 cm, light west wind, alpine temperature -7 C, freezing level below valley bottom.

MONDAY: Mostly cloudy with possible flurries; 0-3 cm, light west wind, alpine temperature -2 C, freezing level 1000 m

TUESDAY: Mix of sun and cloud, light to moderate south wind, alpine temperature -3 C, freezing level 800 m.

WEDNESDAY: Mix of sun and cloud, light to moderate southwest wind, alpine temperature 0 C, freezing level rising to 1300 m.

Avalanche Summary

Numerous size 2 storm slab avalanches were remotely skier triggered on Saturday. These slabs will become increasingly touchy and hazardous as the new snow stacks up and settles into a cohesive slab sitting on top of a fragile layer of surface hoar.

Snowpack Summary

20-35 cm of recent snow has buried a widespread layer of surface hoar (size 5-20 mm.). This layer exists at all elevations. This same layer of surface hoar has been reported as sitting on a thin sun crust on solar aspects which is a particularly nasty combination. The new snow will likely become increasingly reactive to human triggers as it stacks up and settles into a cohesive slab. The early February rain crust down 70-100 cm. is another prominent layer in the upper snowpack that requires monitoring. The mid and lower snowpack are generally well settled and strong.

Terrain and Travel

  • Shooting cracks, whumphs and recent avalanches are strong indicators of an unstable snowpack.
  • Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
  • Be alert to conditions that change with elevation, aspect and exposure to wind.
  • Carefully assess open slopes and convex rolls where buried surface hoar may be preserved.

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.