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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

North Columbia.

Flurries Saturday accumulated at upper elevations along with wind. Use caution around ridge crests and lee terrain features, where deposits will be most reactive and may also hide older, recently buried wind slabs.

Confidence

Moderate -

Weather Forecast

SATURDAY NIGHT: Cloudy with scattered flurries, up to 5 cm accumulation / southwest wind, 20-40 gusting to 55 km/h / alpine low -6 C / freezing level 800 mSUNDAY: Cloudy with sunny periods and isolated flurries, trace to 10 cm accumulation / west wind, 20-40 km/h / alpine high -2 C / freezing level 1600 mMONDAY: Mix of sun and cloud with isolated flurries / southwest wind, 10-15 km/h / alpine high -3 C / freezing level 1600 mTUESDAY: Cloudy with sunny breaks and isolated flurries / south wind, 15-30 km/h / alpine high -2 C / freezing level 1900 m

Avalanche Summary

On Thursday, a few human triggered loose wet avalanches up to size 1.5 were observed on steep slopes in the afternoon. Evidence of a solar-induced wet slab cycle on west aspect around 2400 m was reported on Friday.On Wednesday the avalanche activity decreased. A few natural and human triggered wind/storm slab avalanches up to size 2 were reported on west and north aspects at treeline and in the alpine.On Tuesday, several natural and human triggered storm/wind slab avalanches 20-40 cm deep and up to size 2.5 were observed on north and east aspects. Two of these were remotely triggered, one by humans and another one by a helicopter. A layer of small surface hoar below the most recent snow may have been the weak layer. Several natural wet slab and loose wet avalanches up to size 2.5 were reported from south and west aspects (see a MIN report from Glacier National Park).

Snowpack Summary

Up to 20 cm new snow covers a melt-freeze crust on all aspects except for north facing slopes above 2000 m, where the snow stayed dry. On north-facing aspects in the alpine, the recent 30-50 cm snow was redistributed by wind and, in isolated locations buried surface hoar. Older wind slabs sitting on surface hoar may still be sensitive to human triggers.Below treeline snow is disappearing rapidly.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.