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Avalanche Forecast

Archived

Feb 23rd, 2019–Feb 24th, 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.
Below Treeline
Natural avalanches unlikely.

Regions

Sea To Sky.

Storm slabs are possible to trigger at upper elevations. Use caution on slopes getting hit by the sun.

Confidence

Moderate -

Weather Forecast

SATURDAY NIGHT: Cloudy with clear periods, light southeast wind, alpine temperatures drop to -12 C.SUNDAY: Mix of sun and cloud in the morning and clearing in the afternoon, light northeast wind, alpine high temperatures around -10 C.MONDAY: Sunny, light northeast wind, alpine high temperatures around -12 C.TUESDAY: Sunny, moderate northeast wind, alpine high temperatures around -15 C.

Avalanche Summary

No new avalanches were reported at the time of publishing on Saturday.On Friday, skiers triggered several small (size 1) slab avalanches at upper treeline elevations and in lee alpine terrain. A few small loose dry avalanches were observed on south-facing slopes when the sun came out in the afternoon.

Snowpack Summary

20 cm of low density snow sits above sun crusts on south-facing slopes and hard wind affected snow in the alpine. Deeper deposits may be forming in wind-affected alpine terrain. In sheltered areas, 20 to 40 cm of low-density faceted snow is gradually settling onto old hard surfaces including crusts and wind-packed snow. Low-density snow may sluff easily on these hard surfaces. The lower snowpack is strong and settled.

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.