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Avalanche Forecast

Archived

Feb 23rd, 2012–Feb 24th, 2012

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

Kootenay Boundary.

Confidence

Fair - Timing of incoming weather is uncertain on Friday

Weather Forecast

A low pressure system is moving inland from the coast on Friday. This system is forecast to bring snow and moderate southwest wind to the Columbia Mountains by early morning and to the Kootenay Boundary region by the afternoon. Snowfall amounts are forecast to be about 10 cm for the Purcells and 10-15 cm for the Kootenay Boundary on Friday. Another 10 cm for the Purcells and another 10-15 cm for the Kootenay Boundary are expected overnight and during the day on Saturday. Sunday is forecast to be a mixed bag of convective flurries and some sunny periods. The freezing level is expected to rise to about 700 metres on Friday, drop back to valley bottom overnight and then rise to near 1000 metres on Saturday.

Avalanche Summary

We are getting reports of more frequent and larger avalanches that are running on the Feb. 8th crust and/or buried surface hoar. Avalanches up to size 3.0 were reported from the control work at Kootenay pass along the highway corridor. Remotely triggered avalanches continued to be reported.

Snowpack Summary

About 10 cm on Wednesday night combined with the 10-15 from Tuesday night and strong gusty northwest winds have created widespread windslabs in open areas at all elevations. The snow from the past few days has added to the load which is sitting above the weak layers that developed during the early February drought. There is about 50-80 cm above these persistent weak layers (PWL) of crusts, surface hoar, and facets. Snowpack tests show that the slab above the PWL is sliding easily with sudden planar or sudden collapse characteristics. Professionals throughout the region are treating this layer with extreme caution, since it is showing signs of remote triggering and the ability to propagate in low angled terrain. In shallow snowpack areas concerns remain for the mid-December persistent weakness down around 80-100cm and for basal facets. Treeline snowpack depths are approximately 230 cm.

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.