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Avalanche Forecast

Archived

Jan 17th, 2017–Jan 18th, 2017

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

Regions

Kootenay Boundary.

There is a lot of uncertainty surrounding the intensity of precipitation amounts in the region. Certainly if the freezing level rises in combination with the potential for heavy snowfall and strong winds, the avalanche danger will be elevated.

Confidence

Moderate - Intensity of incoming weather systems is uncertain on Wednesday

Weather Forecast

WEDNESDAY: Snow with 25-40cm of accumulation and rain possible at lower elevations, moderate to strong southwest winds, freezing level around 1300m.THURSDAY: Flurries, accumulations 5-10cm, strong southwest winds, freezing level around 1300m.FRIDAY: Mainly cloudy with the possibility of isolated flurries, light south wind and freezing level around 1000m.More details can be found on the Mountain Weather Forecast.

Avalanche Summary

Conditions are expected to change overnight as a storm moves into the region and new storm slabs develop. As the load increases over the next few days expect the likelihood of deeper buried layers failing to increase under the new load of snow combined with wind and warm temperatures.

Snowpack Summary

A storm is arriving overnight Tuesday and expected to intensify during the day on Wednesday. Expect new storm slabs to develop above existing weak layers described here. Recent cold and clear weather has promoted both faceting of surface snow as well as the growth of surface hoar that has been reported to be up to 15mm in size below treeline. A sun crust has also been reported forming on steep solar aspects. Beneath a variety of old snow surfaces are buried, including wind scoured surfaces and old wind slabs, widespread near surface faceting (sugary snow), surface hoar in sheltered locations, and/or a breakable sun crust on steep solar aspects. The mid-December surface hoar/ facet layer typically sits down 40-70 cm. This layer is still reactive to some snowpack tests in some areas but is currently considered to be dormant or inactive. However, once the snowpack starts to see a big change, like warming, the likelihood of triggering may increase.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.