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

Feb 24th, 2020–Feb 25th, 2020

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 unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

South Coast.

"Not your typical North Shore storm slab," the current avalanche problem involves a weak layer sitting beneath 30-40 cm of recent snow. This problem is expected to persist longer than is usual for the region and requires extra precautions to avoid getting caught off guard.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Monday night: Cloudy. Light to moderate northwest wind. Freezing level 700 m.

Tuesday: Around 5 cm new snow. Moderate west wind. Freezing level 800 m.

Wednesday: Cloudy. Light to moderate northwest wind. Freezing level 1000 m.

Thursday: Cloudy. Light to moderate southwest wind. Freezing level 1100 m.

Avalanche Summary

Explosive control work produced size 1-1.5 storm slabs running on a crust. Skier control work produced minimal results with limited propagation.

Snowpack Summary

30-60 cm of recent snow sits over a widespread layer of surface hoar which may sit on a breakable crust on solar aspects. Surface hoar is an exceptionally weak layer not often seen in this region, and the crust makes an excellent bed surface for avalanches. The recent snow which fell fluffy and light and lacking slab property, is settling into a slab with the aid of mild temperatures and strong winds. 

As an analogy, think of a mattress (slab) resting on standing dominoes (surface hoar) on top of a glass table (crust). Imagine this configuration on a slope. It would not need to be prodded too hard to start sliding.

The remainder of the snowpack is well settled. Depth varies from around 250 to 300 cm at the peaks of the North Shore mountains (1400 m) tapering rapidly with elevation to no snow below 1000 m.

Terrain and Travel

  • Avoid terrain traps such as gullies and cliffs where the consequence of any avalanche could be serious.
  • Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Any steep opening in the trees should be treated as suspect right now.
  • Keep in mind that human triggering potential persists as natural avalanching tapers off.

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.