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Avalanche Forecast

Archived

Feb 20th, 2017–Feb 21st, 2017

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

Regions

Little Yoho.

Enjoy the great skiing but remember that the potential for large human triggered avalanches persists. Conservative route choices remain the theme of the day anywhere that the weak basal facets are present. These conditions will linger for some time.

Weather Forecast

A mix of sun and cloud with a few light flurries are forecast over the next few days. Winds should stay in the light range and temperatures are expected to be in the -3 to -12 range with a slow decrease over the forecast period.

Snowpack Summary

Another 5-10cm overnight with light winds. Isolated soft slab formation near ridge crests in the alpine. Persistent problems remain with the lower half of the snow pack being weak and faceted in thin snow pack areas or near rocky outcrops. Cooler temperatures have helped to stabilize the snow pack below tree line but it is still weak.

Avalanche Summary

Two notable events in the last 24hrs. One was a remotely triggered size 3 avalanche near Cirque peak triggered by a large whumph almost 200m away. The second was two large avalanches triggered by explosives in "the Elevator Shaft" at Lake Louise after numerous smaller explosives had been tried in the previous 24hrs. All ran on the weak facets.

Confidence

Due to the number of field observations

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.