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Avalanche Forecast

Archived

Jan 17th, 2018–Jan 18th, 2018

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

Northwest Inland.

New snow and wind are increasing avalanche danger in the region. Take a cautious approach while the new snow settles and bonds to the surface.

Confidence

Moderate -

Weather Forecast

Wednesday night: Cloudy with flurries bringing 3-7 cm of new snow. Moderate southeast winds.Thursday: Cloudy with continuing isolated flurries and a trace of new snow. Light to moderate southeast winds. Alpine high temperatures to -5.Friday: Mainly cloudy. Light southeast winds. Alpine high temperatures to -5.Saturday: Mainly cloudy with isolated flurries and a trace of new snow. Light to moderate southwest winds. Alpine high temperatures to -6.

Avalanche Summary

Reports from Monday include two small skier triggered avalanches (both size 1). One was a wind slab on a northwest-facing slope under a wind lip and the other was a remotely triggered avalanche on a 50 cm deep surface hoar layer at 1000 m. These small avalanches may be indicators that the upper snowpack has settled into a more reactive slab.

Snowpack Summary

New snow is falling on a temperature crust left over from warm temperatures on the weekend. This crust likely exists well into the alpine. The warm temperatures also settled the upper snowpack, potentially forming a slab above buried weak layers in the top 50 cm of the snowpack. The potential weak layers include a few crusts and surface hoar layers that formed in early January and December. Recent reports suggest the snow is well bonded to most of these layers, but the recent settlement of the upper snowpack may have changed that.

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.