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Avalanche Forecast

Archived

Apr 2nd, 2018–Apr 3rd, 2018

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

Regions

Kananaskis.

The snowpack is a ways off the typical melt-freeze cycle normally found at this time of year. Still feels like winter out there with lots of good skiing to be found.

Confidence

High -

Weather Forecast

Unseasonably cool weather through Thursday will maintain the winter conditions we have been experiencing. Tuesday is expected to be a mix of sun and cloud with isolated flurries. Alpine areas will reach a high of -11 °C with moderate westerly winds. Similar conditions will persist until Friday when a slight warm-up is expected.

Avalanche Summary

No new avalanche activity was observed today.

Snowpack Summary

A few centimetres of fresh snow fell in the past 24 hours. The recent storm snow the we received earlier in the week is settling and beginning to strengthen. Isolated wind slabs are being found in Alpine terrain along ridge crests and gully features but do not extend far down slope. On solar aspects there is a new thin melt freeze crust the developed on Saturday and then the deeper march 15th crust down closer to 50cm. Field tests are showing no results on this crust so far but we are still cautious in bigger south facing terrain. Dig down and evaluate this interface before committing to a feature.

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.

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.