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Avalanche Forecast

Archived

Feb 2nd, 2016–Feb 3rd, 2016

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.

By definition, treeline is rated as moderate. However, be very cautious with steep open slopes and glades at treeline. Human triggering is still possible in these locations.

Weather Forecast

High cloud cover with very light to no precipitation through Thursday. The wind will pick up slightly from the west into the moderate range late on Wednesday.

Snowpack Summary

Wind slabs in alpine and treeline areas. 40-70cm of snow sits over the Jan 6 surface hoar/facet layer and remains reactive to skier triggering. Test results today on the Jan 6 layer were in the hard range. Isolated whumphing on Mt. Field today, likely on the Jan 6 layer.

Avalanche Summary

Lots of evidence of the previous widespread natural avalanche cycle up to size 3 on all aspects with some large propagations around Mt. Field today.

Confidence

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.