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Avalanche Forecast

Archived

Jan 18th, 2019–Jan 19th, 2019

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural avalanches possible, human triggered probable.
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

South Coast.

A bunch more precipitation is forecast for Friday night into Saturday, with changing freezing levels. Best to avoid avalanche terrain if you find 30 cm of snow or more accumulated, as the new snow likely won't bond well to underlying surfaces.

Confidence

Moderate - Freezing levels are uncertain

Weather Forecast

FRIDAY NIGHT: Cloudy with rain below 1500 m and snow above, accumulation 25 mm rain or 25 cm snow, strong to extreme southwest winds, treeline temperature 0 C, freezing level 1500 m.SATURDAY: Cloudy with light snowfall, accumulation 10 to 15 cm, strong southwest winds, treeline temperature -1 C, freezing level 1000 m.SUNDAY: Mostly cloudy, light north winds, treeline temperature -2 C, freezing level 1000 m.MONDAY: A mix of sun and clouds, light northwest winds, treeline temperature -3 C, freezing level 800 m.

Avalanche Summary

No recent avalanche observations were noted in the region. However, it is suspected that a natural avalanche cycle occurred Thursday night during the height of the storm. Another cycle may occur Friday night during the next storm.

Snowpack Summary

Upwards of 70 mm of water equivalent fell on Thursday night!  The freezing level appeared to be around 1300 m, so it is suspected that around 70 cm of snow fell at treeline and alpine elevations and the snowpack is rain-soaked below treeline. More snow is forecasted to fall on Friday night, with a freezing level at 1500 m and peaking around 1800 m but then dropping to 1000 m.At treeline and alpine elevations, all of this snow is falling onto sun and temperature crusts at most elevations and feathery surface hoar in sheltered and shaded areas. The new snow may not bond well to these surfaces. Below this, the snowpack is well-settled.

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.