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Avalanche Forecast

Archived

Jan 1st, 2014–Jan 2nd, 2014

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

Regions

South Rockies.

Confidence

Fair - Intensity of incoming weather systems is uncertain on Thursday

Weather Forecast

Thursday: Cloudy with flurries increasing in intensity throughout the day with 10-15cm of accumulation by Friday morning. Freezing levels in valley bottoms and alpine winds increasing to strong southwesterlies by the evening. Friday: Snow with another 5-10cm of accumulation (or more east of the divide), light to moderate northerly alpine winds and freezing levels in valley bottoms Saturday: Mostly cloudy with isolated flurries, moderate northwesterly alpine winds and treeline temperatures around -10.

Avalanche Summary

No recent avalanches have been reported. Ski cutting on Tuesday near Crowsnest Pass produced no results.

Snowpack Summary

Alpine areas are highly wind-affected with scoured areas, sastrugi, and deep deposits. At treeline, the snowpack is generally well settled, but definitely more stable in the Crowsnest and Elk Valley North than in the Flathead and Elk Valley South where the late-November persistent weakness of surface hoar, crust, and/or facets down 30-70cm has reached the tipping point for rider triggering in a few areas. Check out this video of a recent snowpack test on this layer.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.