Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Jan 10th, 2014–Jan 11th, 2014

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

Regions

Kootenay Boundary.

Confidence

Fair - Intensity of incoming weather systems is uncertain

Weather Forecast

Tonight and Saturday: A strong low pressure system will track over the province tonight leaving heavy precipitation on the region tonight and tomorrow. Around 30 mm in water equivalent is forecasted. This will be accompanied by strong winds from the S during the night and switching from the W during the day. Freezing levels are expected to rise to 1500 m tonight and lower to 1100 m tomorrow. Sunday: Another system is tracking through the province but is not expected to leave significant amounts of precipitation over the region. Moderate W winds should increase in speed during the day. Freezing levels are forecasted to rise back up to 1500 m. Monday: Light to moderate precipitation as a cold front moves across the interior with similar freezing levels.

Avalanche Summary

Several natural dry loose avalanches up to size 1.5 were reported on steep SE aspect. Also, numerous avalanches up to size 1.5 were skier triggered yesterday in the storm snow on E and S aspects. Another similar size avalanche on a N facing slope was skier triggered but is suspected to have run on a surface hoar layer buried down 50 cm.

Snowpack Summary

The significant amounts of snow forecasted tonight and tomorrow, the strong SW winds redistributing this snow and warmer temperatures is increasing the avalanche danger for tomorrow. Windslabs lee of SW winds below ridgetop in the alpine and at treeline will be very touchy and the storm snow in sheltered areas will also need time to settle. Sluffing is expected in steep terrain at all elevation and storm snow could easily run on the newly buried surface hoar in sheltered areas at treeline and below treeline. This surface hoar layer is sitting on a sun crust on S facing aspects in some locations and could be buried around 40 cm deep by tomorrow. The persistent weak layers (PWL) are a concern to avalanche professionals as they have been producing sudden planar results and show good propagation potential when tested. The end of November facet/crust or surface hoar layer down 90 cm (or 50 cm where snowpack is very thin) and the depth hoar or basal facetting are the most worrisome layers. Presently, they do not seem reactive to skier triggering but this situation may change with additional loading, rising temperatures, and strong wind.

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.

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.