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Avalanche Forecast

Archived

Apr 17th, 2024–Apr 18th, 2024

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

Regions

Glacier.

Keep a heads up for areas where the wind has created a fresh slab

It may slide easily on the crust and may gain enough mass to push you off your intended line.

Confidence

High

Avalanche Summary

A field team on Wednesday observed a natural size 2 slab avalanche. This avalanche started at ridge top from a wind loaded pocket and ran far in the steep north facing terrain. Explosive avalanche control on Wednesday was able to produce a sz 1.5 thin windslab from a treeline slide path.

Over the weekend there was a natural avalanche cycle triggered by strong sun and high freezing levels. All observed avalanches were loose/wet and no bigger than size 2.5.

Snowpack Summary

10-20 cms of snow covers a crust that exists everywhere but high north. Recent winds have blown the new snow into wind slabs in immediate lee features.

The Apr 8 crust is down ~30 cms, and was the layer responsible for recent remote & accidentally triggered avalanches. Feb 3rd crust is the dominant midpack layer down ~110cms and still produces isolated planer results when tested.

BTL the snowpack has gone through a number of melt freeze cycles and is in spring conditions.

Weather Summary

High pressure will set up over much of the province bringing clear skies and colder arctic air into the region.

Tonight: Clear with cloudy periods. Nil precip, freezing level at valley bottom.

Thurs: Sun and cloud, Alp high -6°C, light northeast winds, FZL 1600m.

Fri: Sunny with cloudy periods, Nil precip, high -3°C FZL 1800m

Sat: Mix of sun and cloud, no precip. FZL 2200m

Terrain and Travel Advice

  • Be carefull around freshly wind loaded features.
  • Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

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.