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Avalanche Forecast

Archived

Feb 21st, 2020–Feb 22nd, 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 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.

Regions

Sea To Sky.

Overnight snow may not bond well to underlying layers. Maintain a conservative mindset and travel cautiously to avoid the problem.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

FRIDAY NIGHT: Cloudy with snowfall, accumulation 10 to 20 cm, moderate to strong southwest wind, alpine temperature -6 C, freezing level 1000 m.

SATURDAY: Mix of sun and cloud, light to moderate northwest wind, alpine temperature -8 C, freezing level 1000 m.

SUNDAY: Cloudy with snowfall, accumulation 15 to 20 cm, moderate to strong southwest wind, alpine temperature -8 C, freezing level 800 m.

MONDAY: Mix of sun and cloud, moderate west wind, alpine temperature -10 C, freezing level 700 m.

Avalanche Summary

No new avalanches were observed on Thursday. Avalanche activity is expected to increase Friday night into Saturday with the new snow that will fall with strong southwest wind.

Snowpack Summary

Around 10 to 20 cm of snow is forecast to accumulate Friday night and it will fall with strong southwest wind. This snow may form storm slabs at all elevations. The slabs will likely be deepest in lee terrain features near ridges. The snow may overly a weak layer of surface hoar crystals 5 mm in size and near-surface facets at treeline and alpine elevations or a melt-freeze crust on sun-exposed aspects.

The midpack is well-settled.

Faceted snow and crusts exist near the base of the snowpack in much of the region. This layer is dormant at the moment but appears to be most likely a problem on the eastern side of the region, in alpine terrain, and where there is relatively smooth ground (e.g., glaciers, scree slopes, rock slabs).

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Choose conservative terrain and watch for clues of instability.

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.