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Avalanche Forecast

Archived

Apr 14th, 2019–Apr 15th, 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, human triggered possible.
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

South Coast Inland.

5-15 cm of new snow and moderate to strong westerly winds have formed fresh wind slabs reactive to human triggers. Use caution around lee terrain features and steep, convex slopes.

Confidence

High -

Weather Forecast

SUNDAY NIGHT: Mostly cloudy / Light, northwesterly winds / Alpine low -8 C / Freezing level 800 m..MONDAY: Mix of sun and cloud / Light, southwesterly winds / Alpine high -3 C / Freezing level 1600 m.TUESDAY: Mix of sun and cloud / Light, southwesterly winds / Alpine high -2 C / Freezing level 1600 m.WEDNESDAY: Mix of sun and cloud / Moderate, westerly winds / Alpine high 0 C / Freezing level 2000 m

Avalanche Summary

No new avalanches were reported in this region on Saturday.On Friday, a snowmobiler was buried in a size 2.5 wind slab avalanche on a north facing aspect at 2200 m. near the Blowdown cabin. Check out the MIN report HERE.

Snowpack Summary

Currently, the snowpack structure changes dramatically with elevation and aspect. 10-20 cm. of recent storm snow (amounts tapering with elevation) is sitting on a melt/freeze crust, except for north facing terrain above 2000 m. where the old snow surface remained dry and small surface hoar (weak, feathery crystals) may be present in isolated locations. This recent snow has been affected by the sun and re-distributed by southerly winds, forming wind slabs on lee features below ridgetops.Below roughly 1900 m, the snowpack is moist and is melting rapidly at lower elevations. Check out this useful link for managing avalanche hazard during spring conditions HERE.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.