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Avalanche Forecast

Archived

Apr 4th, 2018–Apr 5th, 2018

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

Regions

South Coast.

Winter continues. Snow forecast for Thursday is expected to create storm slabs at upper elevations.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

THURSDAY: Rain to about 1300 m, with up to 25 cm wet snow falling at higher elevations. Moderate to strong southerly winds. Freezing level near 1500 m.FRIDAY: Light snow. Light southerly winds. Freezing level near 1500 m.SATURDAY: Light to moderate snow, falling as rain below treeline. Light winds. Freezing level rising to 1750 m.Weather models disagree on the amount of precipitation expected this week.

Avalanche Summary

No new avalanches have been reported.

Snowpack Summary

Alpine areas around Squamish are expected to develop new storm slabs on Thursday. New snow will add to recent snow which overlies variable surfaces including crusts and facets. Little is known about these buried weak layers, but they are more likely to be problematic on shady aspects. The mid and lower snowpack are generally strong.At treeline and below, a strong spring snowpack exists. Rain may break down surface crusts on Thursday, but the snowpack is expected to regain strength once the temperature drops again.

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.