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Avalanche Forecast

Archived

Nov 22nd, 2019–Nov 23rd, 2019

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

Regions

Glacier.

The new Winter Permit System is in effect.

Ensure you have a permit to enter restricted areas when they are open.

Direct sun and rising freezing levels may increase the likelihood of triggering an avalanche

Weather Forecast

The high pressure ridge is breaking down today. W'ly flow will bring cloud cover ahead of snowfall tonight and push freezing levels to 1100m during the day. On Saturday freezing levels will rise to 1400m with heavy precipitation and SW winds. The storm is due to taper off early Sunday morning with moderate W winds and temperatures dropping.

Snowpack Summary

A 35-50cm persistent slab sits on a crust/surface hoar/stellar layer. Below this are several melt-freeze crusts from late October. Tests are showing easy to moderate results on the persistent slab, indicating they are easily triggered by human loads.

Avalanche Summary

Human-triggered avalanches to size 2 were reported from Little Sifton, Balu Pass and the Asulkan Hut area this week. The Balu Pass avalanche buried the person to their neck and gear was lost. Numerous natural avalanches to size 2.5-3 were observed from The Dome, Tupper, MacDonald, and Cheops during the storm Sunday morning.

Confidence

Intensity of incoming weather systems is uncertain on Saturday

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.