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Avalanche Forecast

Archived

Dec 25th, 2015–Dec 26th, 2015

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

Regions

Northwest Inland.

Strong winds and moderate to heavy snow fall are expected to drive a natural avalanche cycle on Saturday.

Confidence

Moderate

Weather Forecast

Snow is expected to start falling early Saturday morning becoming heavy in the afternoon. Up to 15cm is expected through the day and overnight with another 5 forecast for Sunday morning. Monday looks to be mainly dry. An Arctic front just inland will keep things cool with freezing levels at valley bottom. Strong southwest winds are expected to build on Saturday becoming moderate to light westerlies on Sunday and northeasterly by Monday as a ridge moves inland.

Avalanche Summary

No recent avalanche have been reported.

Snowpack Summary

I suspect that the recent cold temperatures have faceted out the upper snowpack. As of Friday ski pen at treeline was reported to be about 20-30 cm and. This means there is lots of low density surface snow available to blow around when the winds pick up. We're still dealing with a thin, early-season snow pack for much of the Northwest Inland region. Between 80 and 100 cm of snow can be found at tree-line in the south and west of the region, with closer to 60 cm in the east. A weak basal layer probably exists in most areas.

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.