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Avalanche Forecast

Archived

Jan 9th, 2017–Jan 10th, 2017

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.

Continually assess conditions as you travel and watch out for isolated (wind) slabs.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

TUESDAY: Sunny with 20 Km/hr northeast winds. Freezing level dropping to sea level. Treeline temperatures around -4.WEDNESDAY: Sunny with occasional cloud. Light and variable winds. Freezing level at sea level. Treeline temperatures around -7.THURSDAY: Sunny with clouds in the afternoon. Light westerly winds 10-15 Km/hr. Freezing level at sea level. Treeline temperatures around -6.

Avalanche Summary

Only minor loose wet Size 1 natural avalanches were observed yesterday in the North Shore mountains.

Snowpack Summary

The North Shore mountains received 10cm of new snow which came in wet and heavy, bonding well to 15 cm of settling snow from Friday's storm. New snow amounts closer to Squamish were almost double (15-20cm).  Watch out for small wind slabs on north-facing slopes in the lee of exposed features. Friday's snow buried a variable interface composed of faceted (sugary) snow and old hard wind slabs (especially at higher elevations). Recent reports suggest the snow has bonded fairly well to this interface. The mid and lower snowpack are well settled and stable.

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.