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Avalanche Forecast

Archived

Jan 8th, 2013–Jan 9th, 2013

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 unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
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, human triggered possible.

Regions

Northwest Coastal.

Confidence

Fair - Due to limited field observations for the entire period

Weather Forecast

Wednesday and Thursday: Mostly clear with isolated flurries possible. Freezing levels down to seal level and light to moderate northerly winds. Friday: Mostly cloudy with light snow flurries throughout the day, freezing levels at sea level and light westerly winds.

Avalanche Summary

Recent reports are limited, but include minor natural and ski-cut sluffing as well as a couple of Size 1, 10cm deep ski-cut wind slab avalanches.

Snowpack Summary

Another 15-20cm has added to the 40-90cm of storm snow in the past 10 days or so. Weaknesses exist within and under this recent storm snow including touchy surface hoar and/or facets from the end of December under it all. Recent strong southwesterly to easterly winds have set up wind slabs in many exposed lee areas. A deeper surface hoar layer was buried at the beginning of December and is now down well over a metre, but there are no recent reports of activity on this layer. Near the base of the snowpack, a crust/facet layer continues to concern local avalanche professionals. This weakness is unlikely to be triggered by a single person, but it remains possible with a very heavy load (e.g. cornice fall) or from a thin-spot trigger point.

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.