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Avalanche Forecast

Archived

Jan 31st, 2013–Feb 1st, 2013

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

Northwest Coastal.

Confidence

Fair

Weather Forecast

The next frontal system looks to be aimed at the North Coast for Friday bringing generally light precipitation amounts and rising freezing levels. The brunt of the frontal system will take affect through the weekend with temperatures dropping Sunday night.Friday: Light precipitation, snow amounts 5-8 cm above 1000 m. Ridgetop winds light from the SW and moderate SW for areas north of the Portland Inlet. Alpine temperatures -3.0 and freezing levels near 900 m. Saturday: No significant precipitation expected. Cloudy skies with ridgetop winds moderate from the South. Alpine temperatures -1.0 and freezing levels rising to 1300 m. Saturday night into Sunday: The next wave of precipitation bringing light-moderate amounts. Ridgetop winds moderate from the south. Alpine temperatures dropping to -4.0 and freezing levels near 800 m in the afternoon falling to valley bottom overnight.

Avalanche Summary

Natural avalanche activity up to size 2.0 was reported from a NE aspect around 1200 m, suspect cornice fall pulling out the slab on the slope below. Isolated small slabs up to size 1.5 initiated from steep alpine features.Avalanche control work using explosives produced numerous slab avalanches up to size 3.0 in the Northern parts of the region. These ran on NE-S aspects 1300 m and above. Failure planes were ground and within recent storm snow, all on previously controlled slopes.

Snowpack Summary

Wind slabs are most likely found on SE-W aspects, behind terrain features like ridges and ribs, and may be easily triggered under the weight of a person. Warmer temperatures have promoted some settlement and consolidated the recent storm snow into slab-like characteristics. Surface snow may become moist or wet at treeline and below and become unstable.Lingering beneath the new snow sits a persistent weaknesses comprising of surface hoar/ facets/ crust. Recent test done on these layers are producing hard results with sudden and resistant planar results.  I suggest you keep these on your radar in regards to reactivity and sensitivity until we get through the warming period.  If reactive, these layers could produce large avalanches. The mid and lower snowpack is generally well settled and strong, although basal facets remain a concern in the northern part of the region.

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.