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Avalanche Forecast

Archived

Dec 19th, 2018–Dec 20th, 2018

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

As the storm tapers and the weather cools off, the snowpack will begin to gain some strength.  Conservative terrain selection is still recommended, especially in the alpine and upper treeline areas.

Confidence

Low - Due to the number of field observations.

Weather Forecast

WEDNESDAY NIGHT: Cloudy with flurries, 5-10 cm, moderate southwest winds, alpine low temperature near -10°c. THURSDAY: A mix of sun and cloud with isolated flurries up to 5 cm, east to northeast winds, 20-40 km/h, gusting to 60 km/h, alpine high temperature near -5°c, low temperature near -10°c. FRIDAY: Cloudy with sunny periods and isolated flurries, southerly winds, 20-40 km/h, gusting to 55 km/h, alpine high temperature near -6°c, low temperature near -9°c. SATURDAY: Flurries, 5-10 cm, southeast winds, 20-40 km/h, gusting to 55 km/h, alpine high temperature near -4°c, low temperature near -8°c.

Avalanche Summary

Observations have been limited over the past week due to poor weather conditions, but with the enormous amount of snowfall there have likely been several cycles of natural avalanche activity. Several large natural avalanches (size 2-3) were reported in wind loaded alpine terrain near Stewart on Tuesday. A few smaller natural avalanches (size 1-2) were reported in steep terrain in the Shames area over the past few days.

Snowpack Summary

Over the past week an onslaught of storms has delivered 100-150cm of snow to the region. Warm temperatures have left the surface snow moist up to approximately 1000m, which will likely freeze into a crust with dropping temperatures this week. Strong wind has likely affected open terrain at higher elevations and formed thick wind deposits in lee terrain. All of this storm snow sits above an interface that was a concern during the start of the storm, but the strength of this layer has likely improved substantially over the past week. The interface is composed of surface hoar (feathery crystals), facets (sugary snow), and crusts that formed during the dry spell in early December. Deeper in the snowpack, there are several crusts, including an early season crust with facets near the bottom of the snowpack.

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.