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Avalanche Forecast

Archived

Mar 19th, 2021–Mar 20th, 2021

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

Regions

Northwest Coastal.

Steady snowfall and elevated winds are keeping winter alive up high. Be ready to manage a typical array of wind slab and cornice hazards as you gain elevation. Push danger ratings a step higher if you're closer to Bear Pass than Shames.

Confidence

Moderate -

Weather Forecast

Friday night: Cloudy with continuing scattered flurries bringing up to 5 more cm of new snow. Moderate to strong west or northwest winds.

Saturday: Cloudy with a stronger storm pulse starting with a trace of new snow then increasing quite a bit overnight. Moderate west or southwest winds becoming extreme south overnight. Alpine high temperatures around -8.

Sunday: Cloudy with continuing flurries bringing an uncertain 5-15 cm of new snow, closer to 10-30 cm with overnight accumulations. Extreme south winds easing to light southwest in the afternoon. Alpine high temperatures around -6.

Monday: Cloudy with isolated flurries. Light southwest winds. Alpine high temperatures around -5.

Avalanche Summary

Observations from the last couple of stormy days are still limited, however a MIN report from Thursday in the Shames area paints a clear picture of slab reactivity in specific wind loaded features. Similar conditions should persist through Saturday as new snow and wind continue to form surface instabilities.

A natural wind slab avalanche cycle with numerous wind slabs from size 2 to 3.5 (large to very large) was reportedly ongoing in the Bear Pass area on Wednesday morning and again on Friday morning. Natural wet loose and glide avalanches have accompanied this activity below about 900 metres. 

Snowpack Summary

Light new snow amounts will continue to accumulate through Saturday afternoon when a stronger storm pulse begins to move into the region. Elevated winds will likely continue to forming fresh slabs in lee features at treeline before a more widespread storm slab problem forms over Saturday night. Incremental snowfall over the past week added to storm totals from last weekend ranging from 50 cm in the north to 150 cm in the south of the region. Rain fell below 900 m during that storm, saturating the upper snowpack at lower elevations.

Collectively, our new snow and recent storm snow may overlie a persistent weak layer of surface hoar buried March 12 on sheltered northerly aspects around treeline or a melt-freeze crust on southerly aspects and below treeline.

Around 100 to 300 cm now overlies a persistent weak layer buried in mid-February that may still be a concern in isolated parts of the region. The layer consists of surface hoar in areas sheltered from the wind and facets that formed during February's cold snap. 

Conditions are lending themselves to these persistent layers stabilizing, but professionals in the region are continuing to track and treat them with caution, especially the shallower layer from March.

The mid and lower snowpack is well settled and strong in most areas.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Choose conservative terrain and watch for clues of instability.
  • Make observations and assess conditions continually as you travel.

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.