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Avalanche Forecast

Archived

Nov 29th, 2016–Nov 30th, 2016

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

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Wind slab found in the near and above treeline bands will be the primary avalanche problem on Wednesday. Look for signs of recent wind loading on a variety of aspects.

Detailed Forecast

A weak frontal system passing through the Cascades early Wednesday morning should bring light amounts of new snow above 3000 feet.

Previously formed and fresh wind slabs found in the near and above treeline bands and on a variety of aspects will be the main avalanche problem Wednesday. Watch for signs of firmer wind transported snow that indicate wind slab. 

Be aware of a buried surface hoar layer in the Washington Pass zone (see discussion). Reports are few early this season and it's not known how reactive or widespread this layer might be along the east slopes. 

Snowpack Discussion

Weather Discussion for the Cascade East Slopes

A frontal system passed through the Cascades Sunday night and was followed by NW flow aloft on Monday. This pattern favored the west slopes for significant snow accumulations. Near the Cascade crest along the east slopes, snow amounts were in the 3-5 inch range with lesser amounts further east. Moderate WNW winds continued through the day Monday as recorded at the Mission Ridge and Dirty Face weather stations. Tuesday was a fair day with light winds along the east slopes. 

Recent Reports for the Cascade East Slopes

Last Friday a skier triggered a deep wind slab on a 40 degree northwest slope at about 7500 feet on Slate Peak near Harts Pass. The crown varied from about 2 to 7 feet and ran about 2-300 vertical feet with car sized chunks of debris. Fortunately the skier was not caught. He noted that windward slopes across the valley were scoured indicating recent wind transport.

On Tuesday, NWAC professional observer Jeff Ward was in the Washington Pass area. He found generally good ski conditions and a stable snowpack. Previous wind loading was obvious but varied by aspect throughout the terrain. However, wind slabs were stubborn and unlikely to trigger in the drainages he traveled through. 

One layer of interest was buried surface hoar at 65 cm down on a north aspect at 7000 feet. Older avalanche crowns did not seem to step down to this deeper layer. It's not known how widespread this buried weak layer might be but the upcoming weather over the weekend should give it a good load. 

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.