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Avalanche Forecast

Archived

Dec 27th, 2014–Dec 28th, 2014

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.
Below Treeline
Natural avalanches unlikely.

Regions

Sea To Sky.

Be alert to a developing wind slab problem.

Confidence

Fair - Due to the number of field observations

Weather Forecast

Expect light snow on Sunday, then it becomes cold and clear with light to moderate N-NE outflow winds.

Avalanche Summary

On Friday a few size 1-1.5 wind slabs failed in steep terrain. On Wednesday, a snowboarder triggered a size 2-2.5 slab on a north aspect at 1900 m in the Callahan area. The crown was 10cm-100cm deep. The slab is believed to have failed on a crust. The snowboarder was buried, but was recovered safely by companion rescue.

Snowpack Summary

10-20cm new snow overlies large surface hoar crystals which sit above old wind slabs and other variable surfaces. A deeper layer of surface hoar buried in mid-December (now down 40-70cm) has been gradually gaining strength, but may still be a concern in some areas. The mid and lower snowpack contain several old crust layers, one of which may have been the failure layer for a recent burial (see avalanche summary).

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.