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Avalanche Forecast

Archived

Jan 1st, 2013–Jan 2nd, 2013

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

Northwest Inland.

Confidence

Fair - Freezing levels are uncertain on Thursday

Weather Forecast

Wednesday. Mostly dry. Treeline temperatures around -9C. Extreme ridgetop winds gusting to 100km/h from the SW. Thursday: Flurries. Temperatures warming up with freezing levels spiking to around 800m briefly in the afternoon. Ridgetop winds around 60 km/h from the SW. Friday: Flurries. Treeline temperatures around -7C. Ridgetop winds around 40km/h from the SW.

Avalanche Summary

A size 1 avalanche was triggered by a skier on 29th Dec in a pocket of wind slab. I suspect similar events are possible with the current conditions, although there have been no further reports since this event. A natural size 2 slab avalanche was observed in the Hankin area that would have happened around December 28th. Most likely triggered by a cornice fall on a North facing slope, it stepped down deeper in the snowpack, suspecting the November 6th crust. For more information check out the report here.

Snowpack Summary

The snowpack is generally shallow (about 1m deep). and strong winds have scoured some alpine slopes to ground. Wind slabs exist in many wind-exposed areas, however their distribution is quite variable and some areas have no wind-effect at all. It is still possible to find cold, low density snow at the surface in wind sheltered areas. Below treeline, very loose cold snow is sluffing easily from steep terrain and early season hazards like exposed stumps and rocks are still present in places. Professionals are still mindful of a facet/crust layer near the base of the snowpack. Although triggering it has become unlikely, it may be possible from a thin-spot trigger point or with a very heavy load (e.g. cornice fall). A natural slab avalanche that happened on December 28th illustrates that caution is still warranted for this layer.

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.