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Avalanche Forecast

Archived

Feb 24th, 2014–Feb 25th, 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

South Columbia.

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

A strong arctic ridge of high pressure dominates conditions for the forecast period. Clear and dry conditions are expected for the next three days with a bit of a warming trend.Monday night: Clear and cold, treeline temperature around -10C, ridgetop winds light NETuesday: Clear and sunny, treeline temperature around -7C, ridgetop winds light variableWednesday: Clear and sunny, treeline temperature around -6, possiblility of an alpine temperature inversion - ridgetop winds light variableThursday: Sunny with some cloudy periods, possible flurries, light ridge top winds.

Avalanche Summary

We have been receiving less reports of natural activity in the last couple days, but the natural avalanches that are occurring have been increasing in size. On Sunday there were several natural size 2 avalanches reported in the region.Conditions are ideal for human triggering right now and we have received numerous reports of skier triggered avalanches, many of which have released quite deep in the snowpack. Several of these avalanches were remotely triggered. On Sunday we received two reports of remotely triggered avalanches in the South Columbias. The largest of these were size 2, the deepest was 120cm, and the farthest remote trigger was 100m away.

Snowpack Summary

A cohesive slab with an average thickness of 1m 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 creating problems even in previously skied terrain. Large settlements and whumpfs have been reported at all elevations. We have received numerous reports of remotely-triggered avalanches from as far as 500m away, indicating a high likelihood of large propagation within the weak layer. Touchy conditions are expected to remain in place longer than we're normally accustomed to. Recent strong winds out of the SW through NW have created wind slabs on lee features in wind exposed areas at treeline and above. In many wind loaded areas, a slab of up to 2 m thickness overlie the persistent weak layer creating conditions for very large avalanches.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.