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Avalanche Forecast

Archived

Dec 6th, 2015–Dec 7th, 2015

Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.
Alpine
Natural and human triggered avalanches likely.
Treeline
Natural and human triggered avalanches likely.
Below Treeline
Natural avalanches possible, human triggered probable.

Regions

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Back country early season conditions are changing fast! The forecast has been updated early Sunday morning for dangerous conditions. Back country travel is not recommended Sunday near and above treeline in the Mt Baker area on Sunday.

Detailed Forecast

Strong alpine winds and moderate to heavy rain and snow will accompany a cold front across the Northwest Saturday afternoon to Sunday morning. This should bring 1-2 feet of new snow near and above treeline with the most expected in the Mt Baker area with a warming trend which greatly increases the likelihood of storm and wind slab layers.

Back country early season conditions are changing fast! New potentially large storm and wind slab will be the focus on Sunday especially in the Mt Baker area but also along the entire west slopes. Human triggered storm slab should be likely to very likely on varied aspects. Human triggered wind slab should be likely to very likely mainly on lee north to east slopes especially above treeline. Back country travel is not recommended Sunday near and above treeline in the Mt Baker area.

The next strong system should begin to move into the Olympics and Cascades Sunday night. But be prepared to curtail your plans later Sunday if conditions deteriorate sooner than expected.

Snowpack Discussion

Note: The snowpack discussion is for the entire west slopes of the Cascades but the avalanche danger forecast varies by zone.  

We had a wild and wet month of November, with 12- 25 inches of water at west side NWAC stations only amounting to about a 1 meter or 3 foot snowpack in the north Cascades above 4000 feet and above 6000 feet elsewhere. Then strong high pressure led to strong temperature inversions and brought very cold air through the Cascade Passes over Thanksgiving weekend. The weather pattern has become more active for the first few days of December with a few inches of new snow over the west slopes paired with moderating temperatures in the Passes. 

Update Sunday morning: There has now been about 1-3 feet of snow with an overall warming trend since the start of the month along the west slops with the most at Mt Baker. New NWAC pro-observer Simon Trautman was near the Mt Baker Ski Area on Saturday and reported reactive upside down P hardness wind slab over lower density layers with numerous natural storm slab avalanches and some remote ski triggered wind slab avalanches up to about 15 inches. The avalanche danger forecast for the west slopes of the Washington Cascades has been nudged up due due to this new information.

The west slopes do not have a uniform maritime snowpack! Due to the cold temperatures and clear skies near the end of November, buried surface hoar can be found in the Stevens Pass area. NWAC pro-observer Dallas Glass found this layer at 4-5000 feet at Skyline on E-NE aspects around 45 cm down. Faceting may also be found at a similar depth on solar aspects around a buried sun crust.  Stevens pass pro patrol reported a 12-14 inch (30-35 cm) natural persistent slab avalanche in closed Corona Bowl of the ski area Friday on a N-NW aspect.  Professionals also reported shooting cracks and whumpfing in the area as temperatures warmed and the slab above the PWL became cohesive.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.