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Avalanche Forecast

Archived

Dec 20th, 2017–Dec 21st, 2017

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

Regions

Purcells.

Choose conservative terrain in the coming days as recent storm slab continues to settle and consolidate.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

THURSDAY: Cloudy with flurries, accumulations 5cm / wind light to moderate northwest / alpine temperature -8FRIDAY: Mix of sun and cloud / wind moderate north / alpine temperature -10SATURDAY: Mainly sunny / wind moderate northwest / alpine temperature -11

Avalanche Summary

Recent reports indicate a few size 1-1.5 remote triggered (triggered from a distance) avalanches in the alpine and tree line. These are isolated to this past week's storm snow. Additional reports show natural wind slab avalanches to size 2 in the alpine on north and east aspects in the alpine along with skier triggered and natural size 1 loose snow avalanches in steep terrain at tree line and in the alpine. As snow amounts continue to settle and consolidate in the coming days, expect to see avalanche activity continue.

Snowpack Summary

20-50cm of new snow accumulating over the past week sits on a wide variety of old surfaces including large surface hoar (weak, feather-like crystals), hard crusts formed by sun or wind, and sugary facets. As the snow load builds and slab properties develop, it will be important to monitor how the new snow is bonding to the old surfaces. Most concerning would be areas that have had previous surface hoar development, such as sheltered areas at and below tree line and/or sheltered northerly aspects in the alpine. A crust which was formed by rain in late November is a major feature in the snowpack and is down approximately 40-60cm at tree line elevations. Snowpack tests suggest the snow above is currently bonding well to it.Snowpack depth decreases rapidly below tree line. Look out for early season hazards such as rocks, stumps, and open creeks.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.