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Avalanche Forecast

Archived

Dec 26th, 2017–Dec 27th, 2017

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

Regions

Glacier.

Cold temps and light winds have preserved the excellent snow quality.Assess the snowpack before entering your line.Happy Holidays!

Weather Forecast

A strong ridge of high pressure is keeping cold Arctic air sitting over most of BC. The winds will be 5-15km/hr from the Southwest  with no snowfall expected. Today we will see an alpine high of -16 deg C, that's the warmest it'll get, bring an extra layer or two and stay in the sun!  Looks like snow and warmer temps are on the way Friday ....maybe

Snowpack Summary

Cold temps are facetting the surface snow and keeping it soft & unconsolidated. Below tree line 40cm sits on the Dec 15 layer surface hoar which is widespread and largest where sheltered. In the alpine, Dec 15 is a thin crust on solar aspects and small surface hoar on polar aspects. Pockets of wind slab exist in the alpine and at tree line.

Avalanche Summary

No new avalanches observed yesterday.Numerous natural avalanches from a few days ago up to sz 2.5 in steep terrain.

Confidence

Wind effect is extremely variable

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.

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.