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Avalanche Forecast

Archived

Feb 27th, 2017–Feb 28th, 2017

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

Regions

Little Yoho.

Ski and climbing conditions are good right now, and we have seen less avalanche activity over the previous few days. However we remain wary of the weak snowpack that dominates the region. Consider your exposure to avalanche terrain very carefully.

Weather Forecast

One more day in this same, stable weather pattern before things change. Tuesday expect temperatures ranging from -15 to -25, light winds and no new snow - looks like another nice day and then on Tuesday night the wind picks up and the remainder of the week will be snowy. Expecting 10-15 cm through the second half of this week.

Snowpack Summary

30cm of soft snow overlies a well-settled and firm middle of the snowpack. Near treeline, concern remains for a facetted layer that sits in the lower third of the snowpack, and an old surface hoar layer down about 50-60 cm that has recently produced sudden planar shears. Deeper snowpacks to the west of the Wapta Icefields have the strongest snow.

Avalanche Summary

No new avalanches were observed or reported on Monday.

Confidence

Problems

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.