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Avalanche Forecast

Archived

Dec 24th, 2016–Dec 25th, 2016

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

Regions

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Wind slab may be still be sensitive on lee slopes mainly near and above treeline, especially where poorly bonded to an underlying crust. While the 12/17 PWL is gaining strength and appears increasingly unlikely to be human triggered, remember that persistent weak layers are generally involved in larger avalanches and above normal caution is still advised.

Detailed Forecast

Christmas should be cold and mostly sunny with generally light winds across the Cascade range. 

Shallow wind slab formed Thursday and Friday has become less likely to trigger. However, wind slab may be locally more sensitive in areas it has poorly bonded to an underlying crust.   

The latest tests of the December 17th PWL in the Cascades don't seem to indicate a regionally reactive layer. There is still some uncertainty regarding this layer but we are gaining confidence that it is less of an issue and have moved the likelihood down a notch to Unlikely. 

However, since this layer is still showing the ability to propagate in snowpack tests throughout much of the range, we still advise observing the snowpack structure in your local area and skiing or riding on lower angled slopes until there is more certainty that this layer is no longer a problem. While triggering this layer seems unlikely, remember that persistent weak layers are generally involved in larger avalanches.

Storm slabs that were reactive in the Mt. Baker area Friday should have settled out by Sunday and storm slabs will not be listed as an avalanche problem. 

The surface crust formed last week is strong and hard enough in some areas of the west slopes to present an out of control fall danger. Avoid steep slopes where the slide for life hazard is present. 

Snowpack Discussion

Weather and Snowpack

Strong westerly flow directed two Pacific frontal systems across the Northwest last Sunday night and again Monday night (12/18-12/19) with generally 1 to 2 inches of water accumulating along the west slopes through early Tuesday morning. A period of rain during this storm cycle allowed crust layers to form in the Baker area from 4000-4500 feet, the Passes up to around 5000 feet (Stevens) to 6000 feet (Snoqualmie) and 6000-7000 feet in the Paradise area. In most areas the crust is strong enough to support a skier's weight.

After a fair weather period midweek another front crossed the Northwest on Thursday followed by an upper trough on Friday with low snow levels. About 20 inches of snow accumulated at Mt. Baker over this period with about 2-8 inches accumulating elsewhere along the west slopes including the Passes. 

Scattered snow showers, sunbreaks and generally light winds summed up the weather on Saturday. 

Recent Observations

Several worthwhile observations are available for the west slopes from Wednesday through Thursday, 12/21-12/22 ,via the NWAC Observations tab. In summary no avalanches or direct signs of deeper instability were reported, however the 12/17 PWL showed some propensity for propagation in snowpack tests. 

NWAC pro-observer Lee Lazzara was out in heavy snowfall on south slopes on Mt Herman near Mt Baker on Friday in the 4-5000 foot range and reported widespread reactive 15-30 cm storm slab releasing on a recent storm interface. Lee did not find the December 17th PWL in a pit on a north slope. The 12/17 layer was identified but unreactive in snowpack tests at about 70 cm on a south slope.

The Alpental pro-patrol on Friday and Saturday reported shallow wind slab on wind loaded areas which was poorly bonded to the crust formed last week. Elsewhere new snow was not cohesive and was sluffing on the crust. Sensitive and shallow wind slab was also reported in the Silver Basin area of Crystal Friday. 

Pro-observer Ian Nicholson was at Mt. Snoqualmie Saturday morning. Ian identified shallow wind slab as his greatest potential concern on steeper wind loaded slopes where it had bonded poorly to a graupel layer overlying the uppermost crust. The 12/17 PWL was showing signs of propagation in snowpit tests, but was requiring more load and showed signs of rounding versus earlier in the week.  

Crusts in the Snoqualmie Pass and Paradise area have been reported as especially stout with ski crampons helpful on steeper slopes. 

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.