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Avalanche Forecast

Archived

Feb 25th, 2020–Feb 26th, 2020

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 unlikely, human triggered possible.
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

South Coast.

A weak layer atypical of this region sits beneath a 30-60 cm thick storm slab. It is most prevalent on shady (north-facing) aspects at upper elevations. Avoid terrain traps and approach convexities and wind loaded features with caution.

Confidence

Moderate - Uncertainty is due to how quickly the snowpack will recover and gain strength.

Weather Forecast

Tuesday night: Cloudy. Light to moderate west wind. Freezing level 800 m.

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

Thursday: 5-10 cm new snow. Moderate southwest wind. Freezing level 1300 m.

Friday: Mix of sun and cloud. Light southwest wind. Freezing level 1700 m.

Avalanche Summary

This MIN post from Monday reports a skier triggered size 1 wind slab in the alpine, suspected to have run on surface hoar. Explosive control work conducted Monday produced size 1-1.5 storm slabs running on a crust.

Snowpack Summary

30-60 cm of recent snow sits over a layer of surface hoar on north-facing (shady) aspects. There may also be areas where the surface hoar sits on a crust, which makes an excellent bed surface for avalanches. Surface hoar is an exceptionally weak layer not often seen in this region. It is expected to persist at least through the week. It is buried deep enough that it is stubborn to human triggers, but may be reactive where overlying snow depths vary due to wind.

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

  • Be alert to conditions that change with aspect and elevation.
  • Keep in mind that human triggering potential persists as natural avalanching tapers off.
  • 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.
  • Be carefull around freshly wind loaded features.
  • Caution around convexities or sharp changes in terrain.

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.