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Avalanche Forecast

Archived

Mar 12th, 2019–Mar 13th, 2019

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

Northwest Inland.

The snowpack needs to adjust to it's new load. The best, and safest riding will be in wind protected areas.

Confidence

Moderate -

Weather Forecast

TUESDAY NIGHT: Light west wind.. Treeline temperatures around -10 C. Dry.WEDNESDAY: Light to moderate south wind. Mostly cloudy. Dry. Treeline temperatures -5 to -10 C. THURSDAY: Moderate to strong southwest wind. 5 to maybe 10 cm new snow. Treeline temperatures around -10 C. Mix of sun and cloud.FRIDAY:  Light to moderate south wind. Trace to 10 cm new snow. Warming temperatures with treeline approaching zero. Cloudy.

Avalanche Summary

Few observers in the field Monday but reports are consistent with a natural avalanche cycle of storm slabs and wind slab up to size 2.

Snowpack Summary

The region received 15 to 30 cm of storm snow accumulations on Monday. It covered previously scoured surfaces and old hard wind hammered snow, sun crusts on solar aspects, and sugary facets pretty much everywhere.February's cold weather weakened the upper- and mid-snowpack. In some sheltered areas, 20-50 cm of the snowpack was faceting, or sits on facets (sugary snow),In the south of the region, the lower snowpack is generally strong.

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.