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Avalanche Forecast

Archived

Jan 10th, 2015–Jan 11th, 2015

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

Regions

Little Yoho.

Touchy buried surface hoar from Dec 18th, and widespread propagations on this layer, indicate the need to avoid avalanche terrain for a little while.

Weather Forecast

Moderate alpine temperatures between -5 and -10'C with light winds out of the NW and a mix of sun and cloud are expected for the next several days.

Snowpack Summary

Continuous widespread whumphing in Yoho indicates that the surface hoar on the rain crust problem down 45cm has not changed significantly since the last storm. Wide propagations indicate a good slab formation even below tree line. Areas of wind slab overlying weak facets near ridge tops and in exposed alpine areas are also prone to failure.

Avalanche Summary

Natural avalanche activity has tapered off but human triggering remains likely. A size 1.5 skier triggered avalanche occurred in the Wizard Chutes near tree line Jan 10th in the Sunshine area. Avalanche control at Lake Louise on Jan 9th resulted in a size 3 which initiated on the Dec 18th interface and then stepped down to facets near the ground.

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.

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.