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Avalanche Forecast

Archived

Apr 13th, 2019–Apr 14th, 2019

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

Regions

Kootenay Boundary.

Snowfall Saturday accumulated at upper elevations. Use caution around ridge crests and lee terrain features, where deposits will be most reactive.

Confidence

Moderate -

Weather Forecast

SATURDAY NIGHT: Flurries continuing into the evening, up to 10 cm snow / west wind, 20-40 km/h / alpine low -6 C / freezing level 700 mSUNDAY: Mix of sun and cloud with flurries, trace to 5 cm accumulation / west wind, 20-40 km/h / alpine high -5 C / freezing level 1600 mMONDAY: Mix of sun and cloud and isolated flurries / southwest wind, 10-20 km/h / alpine high -2 C / freezing level 1600 mTUESDAY: Clear with cloudy periods / southwest wind, 10-25 km/h / alpine high +1 C / freezing level 2000 m

Avalanche Summary

On Wednesday, wind slabs in lee features were reactive to explosives.On Tuesday, wind and storm slabs up to size 1 were reactive to skier traffic on sun affected slopes in the alpine.

Snowpack Summary

Up to 15 cm new snow covers a melt-freeze crust on most aspects except for north facing slopes above 2000 m, where new snow overlies dry, settled snow. At these sheltered upper elevations, the recent 10-35 cm snow over the past week is bonding well to the underlying layers.Below treeline snow is disappearing rapidly.

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.