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Avalanche Forecast

Archived

Feb 5th, 2017–Feb 6th, 2017

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

Regions

Little Yoho.

By Monday morning we expect up to 20cm of snow in the forecast region. Ice climbers should consider routes with no overhead hazard until the storm snow has a chance to settle.

Weather Forecast

Small amounts of precip and cold temperatures are expected overnight Sunday and throughout Monday.  Wind will be variable in direction and remain in the light to moderate range.

Snowpack Summary

Little Yoho has received between 10 and 30cm of storm snow. This sits on previous hard surfaces from winds last weekend. A generally weak snowpack exists below 2000m. At 2000m there is about 150cm with the Jan 17 surface hoar layer down 40cm. Deeper snowpack areas closer to the Wapta have a much more solid snowpack.

Avalanche Summary

One size 1 avalanche was observed in the Dennis 1 slide path above the Field Back-road today.

Confidence

Forecast snowfall amounts are uncertain on Monday

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.

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.