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Avalanche Forecast

Archived

Feb 26th, 2014–Feb 27th, 2014

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

Regions

Cariboos.

The hazard may increase with rising temperatures and solar warming on South aspects. See the forecasters blog for more information on current tricky conditions.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

The arctic ridge of high pressure dominates conditions for the forecast period. Clear and dry conditions with cold arctic air scheduled to move back into the region. Strong arctic outflow winds have already begun and will continue into the coming weekend.Wednesday night:  freezing level at valley bottom, ridge top winds light-variable.Thursday: Sunny with some cloudy periods, freezing level around 1400m, ridge top winds, light to 25Km/h.Friday: Sunny, freezing level at valley bottom, ridge top winds from the north to 20 Km/hSaturday:  Freezing level at valley bottom, light ridge top winds from the north.

Avalanche Summary

We're still receiving  reports of large natural avalanche activity in the forecast region. One operator has reported evidence of a recent avalanche cycle in steep terrain with avalanches up to size 2.5.  Solar warming on steep south aspects may trigger avalanches that might "step down" to weak mid -pack and basal layers possibly triggering a very large slide. Conditions are ideal for human triggering right now.  We have received numerous reports of skier triggered avalanches in the last few days, many of which have released quite deep in the snowpack. Several cornice failure avalanches have been reported.

Snowpack Summary

A dense slab with an average thickness of 1.5 metre sits on a nasty persistent weak layer (surface hoar/facet/crust combo) that was formed during the preceding month of cold, dry weather. This weak layer is widespread at all elevations and aspects, and is reactive even in previously skied terrain. Large settlements and whumpfs have been reported at all elevations. We have received numerous reports of remotely-triggered avalanches indicating the ability of this weak layer to fail and propagate over large distances. Touchy conditions are expected to remain in place longer than we're normally accustomed to. Some Katabatic (down-flowing) winds slab formation is being reported as well.Recent strong winds out of the SW through NW have created wind slabs on lee features in wind exposed areas at tree line and above. In many wind loaded areas, a slab of up to 2 m thickness overlies the persistent weak layer creating conditions for very large avalanches.Weak basal facets exist in some areas, but triggering has now become unlikely. For the most part, the mid and lower snowpack are strong and well consolidated.

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.