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Avalanche Forecast

Archived

Feb 10th, 2021–Feb 11th, 2021

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

Regions

South Coast.

Keep your guard up if you're accessing the alpine, where observations remain limited. Watch for wind slabs perched on steep features and note that our recent persistent slab problem may not be beyond triggering where firm layers aren't bridging over it.

Confidence

Moderate -

Weather Forecast

Wednesday night: Clearing. Light east or northeast winds.

Thursday: Sunny. Light northeast winds. Alpine high temperatures around -13.

Friday: Mainly cloudy with light flurries beginning overnight. Light northeast winds. Alpine high temperatures around -9.

Saturday: Cloudy with continuing flurries bringing about 10 total cm of new snow, easing overnight. Light northeast winds. Alpine high temperatures around -8.

Avalanche Summary

There have been no reports of avalanche activity in the region since early last week when a widespread natural avalanche cycle up to size 3 (very large) took place in the North Shore mountains. Dense bridging layers of snow and crust are expected to have effectively neutralized the problem since that time, although some uncertainty exists with regard to higher alpine locations.

Snowpack Summary

A thin skiff of new snow now exists above a mix of breakable surface crust, wind-affected snow, and old wind slabs that have been losing cohesion under the influence of prolonged cold temperatures. A few cm below this surface, a more supportive crust solidly caps the snowpack below about 1400 metres. This crust may be absent at higher elevations.

100-150 cm of snow sits over a widespread persistent weak layer. This weak layer consists of a thick crust with weak facets and/or surface hoar on top of it in many areas. In most areas where it remains preserved, this layer has become difficult to trigger due to bridging by overlying dense snow and crusts. There is some concern for the possibility of continued reactivity in steep terrain at high elevations where it has not previously avalanched and where the overlying snowpack may have failed to form an effective bridge over it.

Click here to watch North Shore Rescue's snowpack conditions update from Friday.

Terrain and Travel

  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and unsupported terrain features.
  • Carefully evaluate steep lines for wind slabs.

Problems

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.