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

Mar 25th, 2020–Mar 26th, 2020

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kootenay Boundary.

Recent snow and wind may form unstable snow on isolated terrain features.

Confidence

Low - Uncertainty is due to limitations in the field data.

Weather Forecast

Wednesday night: Mostly clear, light northwest wind, freezing level valley bottom, alpine temperatures -13 C.

Thursday: Sunny with a few clouds in the afternoon, light southwest wind, freezing level climbing to 1500 m in the afternoon, alpine temperatures reach -5 C.

Friday: Mix of sun and cloud, light southwest wind, freezing level climbing to 1500 m in the afternoon, alpine temperatures reach -3 C.

Saturday: Mix of sun and cloud, isolated flurries with trace accumulations, light southwest wind increasing to moderate, freezing level climbing to 1700 m, alpine temperatures reach -1 C. 

Avalanche Summary

No recent avalanches have been reported, but mountain travel and field observations have been very limited over the past few days. Recent snow could form thin wind slabs with the potential to be reactive above the surface hoar that formed over the past week.

Snowpack Summary

Up to 10 cm of snow fell in the eastern half of the region. This snow sits above a variable mix of crusts, moist snow, and hard old wind slabs. It may also sit above some small surface hoar on shaded aspects. There is some uncertainty about how well the new snow will bond to these interfaces. Weak layers in the upper snowpack have trended towards dormancy. The most prominent and widespread layer was buried in late February and is now 40 to 80 cm deep. This layer was most commonly found in open trees and has produced a few isolated avalanches over the past month.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid terrain traps where the consequence of any avalanche could be serious.

Problems

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.