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Avalanche Forecast

Archived

Dec 23rd, 2012–Dec 24th, 2012

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

Regions

Purcells.

Lower danger ratings in the alpine should not be seen as carte blanche for bigger terrain.  See the forecaster's blog for some ideas about approaching the mountains this week.

Confidence

Good

Weather Forecast

Monday: Light ridgetop winds out of the E. No Snow. 1500m temp: -15 Freezing level: SurfaceTuesday: Light SE ridge top winds. 1500m temp -13 No snow. Freezing Level: SurfaceWednesday: Light SW ridge top winds. Treeline temp -13. No snow. Freezing Level: Surface

Avalanche Summary

No large avalanches were reported yesterday.  There were however a few reports of both natural and skier triggered avalanches to size 1.5 in wind loaded features.  Cornices were also reported to be touchy in the north of the region.

Snowpack Summary

In the last four days the north of the region received 30 - 50 cm while the zone closer to the Purcell Wilderness Conservancy received closer to 80 cm. Winds picked up Wednesday/Thursday of last week forming large wind slabs in the Alpine that produced a limited avalanche cycle to size 2 that persisted through Friday.  It sounds like these slabs are settling out but I'm still suspect of them, especially on steep unsupported features. New (relatively) thin wind slabs involving Saturday nights snow may still be an issue Monday. Cornices are also a problem at the highest elevations. The mid-pack is reported to be settling well. I haven't heard of any test results involving the late November surface hoar in the last five days. The early November crust, near the base of the snowpack has also been inactive as of late. It's important to note that professionals are still cautious about these lingering persistent slab problems, but the likelihood of triggering is low. Be wary of steep complex terrain with a shallow snowpack, where triggering a persistent weakness is more likely.

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.

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.