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Avalanche Forecast

Archived

Mar 13th, 2016–Mar 14th, 2016

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

Regions

Little Yoho.

An intense but short-lived storm last night and an expected dose of snow tonight, will keep windslabs fresh at Treeline and above. Triggering a windslab could have high consequences with the deep persistent slab problem still lingering.

Weather Forecast

Another 5 cm is expected to arrive Sunday night with light to moderate SW winds. Following this freezing levels are expected to drop a bit to 1300m while the light to moderate westerly flow bring trace amounts over the next couple of days .

Snowpack Summary

Widespread wind effect treeline and above with 20 to 35 cm of new snow sitting on a well settled mid and lower pack. This new snow overlies a temperature crust below 1800m on polar aspects and a sun crust into the alpine on solar aspects. No significant shears found in the mid and lower pack, however thin snowpack areas are still suspect.

Avalanche Summary

A few significant avalanches occurred today: a sz 3  on Mt Buller in the K-country at 2300m on a NW aspect, a sz 2.5 was reported at 2400m on a North aspect on Mt Lougheed, both of these were reported as natural windslabs triggering deep facets. A skier triggered sz 2.5 occurred on a West slope near the Sunshine Village ski area on deep facets.

Confidence

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.