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Avalanche Forecast

Archived

Jan 25th, 2015–Jan 26th, 2015

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

Regions

Little Yoho.

A natural avalanche cycle occurred today due to the warm temperatures. We expect this to continue until things cool down. Until then avoid all avalanche terrain and minimize your exposure to large slopes when traveling at valley bottom.

Weather Forecast

Continued warm temperatures with freezing levels near ridge tops and strong to extreme W winds continue for Monday. On Tuesday things begin to cool off slightly and we may see some light precipitation. Wednesday the cooling trend continues with winds shifting to the North and generally clear skies.

Snowpack Summary

Strong to extreme SW winds creating wind slabs in open areas above tree line and intense wind transport at ridge tops. Moist snow to ridge top on solar aspects and on all aspects below tree line. Dec 18th surface hoar failing naturally in some locations and producing avalanches up size 2.5 today.

Avalanche Summary

Numerous natural avalanches were observed and reported today with slabs up to size 2.5 at tree line and above and loose wet slides up to size 2 below tree line in all of the forecast region. Notably Cascade Falls, Rogans Gully, Bourgeau L & R and many of the climbs in Field all saw avalanche activity today. We expect this cycle to continue tomorrow

Confidence

Freezing levels are uncertain on Tuesday

Problems

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.