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Avalanche Forecast

Archived

Mar 27th, 2020–Mar 28th, 2020

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

Regions

South Coast Inland.

New snow and strong wind will create dangerous avalanche conditions. 

Confidence

Low - Uncertainty is due to limitations in the field data.

Weather Forecast

Friday night: Cloudy, scattered flurries with trace accumulations, moderate to strong southwest wind, freezing level dropping to 1200 m, alpine temperatures reach -4 C.

Saturday: Cloudy, 10-20 cm of new snow, moderate southwest wind gusting strong at ridge-tops, freezing level climbing to 1600 m in the afternoon, alpine temperatures reach -2 C.

Sunday: Cloudy, 5-15 cm of new snow, moderate southwest wind gusting strong at ridge-tops, freezing level climbing to 1400 m in the afternoon, alpine temperatures reach -6 C.

Monday: Cloudy, 5-15 cm of new snow, moderate southwest wind, freezing level climbing to 1200 m in the afternoon, alpine temperatures reach -6 C.

Avalanche Summary

No recent avalanches have been reported, but mountain travel and field observations have been very limited over the past few days. Last week there were many wet loose avalanches and some large glide slabs, but cooler weather and new snow has made storm slabs the main concern.

Snowpack Summary

Periods of heavy snow with strong southwest winds are expected to build widespread, reactive storm slabs and create dangerous avalanche conditions. 

Snowfall from earlier in the week was highly variable across the region with some areas receiving 15-25 cm and adjacent valleys getting as little as 0-5 cm. Some of the heavier accumulations fell in the south part of the region. This snow covered a variety of previous snow surfaces including crusts, warm snow, and wind-affected snow. It may also sit above some small surface hoar on shaded, sheltered slopes. Overall, there is some uncertainty about how well the snow has bonded to these interfaces.

Northern parts of the region have had a deep instability lingering at the base of the snowpack for most of the season, however this layer has gained strength over the past month (with the last reported avalanche on Feb 17).

Terrain and Travel

  • Storm slab size and sensitivity to triggering will likely increase through the day.

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.