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Avalanche Forecast

Archived

Dec 17th, 2017–Dec 18th, 2017

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

Regions

Snoqualmie Pass.

The avalanche danger will peak Sunday night through Monday morning during the period of heaviest loading, slightly decreasing later in the day. The snow-line through this period will determine the sensitivity and depth of storm and wind slabs. Expect rising avalanche danger with an increase in elevation, and avoid traveling below paths connected to higher start zones.

Detailed Forecast

The avalanche danger will peak Sunday night through Monday morning during the period of heaviest loading, slightly decreasing later in the day and tapering from north to south across the Cascades. The snow-line through this period will determine the sensitivity and depth of storm and wind slabs. Expect rising avalanche danger with an increase in elevation, and avoid traveling below paths connected to higher start zones. The most significant snowfall is expected at higher elevations of the near and above elevation bands, and moderate to strong W-SW winds will easily transport new snow to lee slopes. A locally lower snow level at Mt. Baker will increase the likelihood of storm slabs developing below treeline. Storm slabs may develop in the upper portion of the below treeline band from Stevens Pass and south to Mt. Rainier. 

Generally small loose wet avalanches are possible at lower elevations in steep terrain.  Be especially careful of even small loose wet avalanches around terrain traps. 

Remember that beneath any new snow received during this storm, a myriad of early season terrain hazards exist, especially at lower elevations. Expect terrain hazards with poorly covered rocks, vegetation and creeks, particularly on south-facing terrain, at lower elevations, and on exposed ridges where wind events have stripped much of the seasons snowcover.

Snowpack Discussion

After 12 long days of high pressure, the first frontal system in quite awhile crossed the Cascades on Friday. New snow accumulations Saturday morning ranged from 2-5 inches along the west slopes of the Cascades with a local maximum at the top of Alpental with 8 inches of new snow. Below this storm snow, a highly varied array of  snow conditions exist, including melt-freeze crusts, settled old storm snow, and a mix of recently formed surface hoar or near surface facets (sugary snow) at lower elevations and some shaded terrain.

Warm frontal moisture that arrived on Sunday brought light rain to 4000-4500 feet in the north Cascades, a battle between rain and wet snow at Stevens and Snoqualmie Passes with light snowfall accumulating at the top of Alpental, and a mix up to about 5500 feet in the south Cascades (Paradise, Crystal) through 4 pm Sunday.  No significant avalanche activity was reported. The warmer temperatures and light rain likely helped wet or potentially destroy recently buried persistent weak layers at lower elevations, especially in the Stevens Pass area.   

The overall snowpack of 2-5 feet along the west slopes is stable with settled old snow sitting over the strong Thanksgiving rain crust, buried about 1.5-2.5 feet.

Observations

North

Baker pro-patrol reported no avalanche concerns in their area Sunday morning.  

Central

Both Stevens and Alpental pro-patrol reported a few small loose wet avalanches localized to very steep terrain features, but otherwise no avalanche activity in area. 

Alpental pro-patrol reported sensitive but shallow 4-6" storm slabs during Saturday morning's avalanche mitigation. The storm slabs were easy to trigger but did not run far. Wind transported snow was noted near-treeline from N-NW winds Friday night.

There is a pertinent observation from the Yodelin area of Stevens Pass from Friday detailing recently buried surface hoar in an open location below treeline on the NWAC observations page.

South

Professional observer Jeremy Allyn was in the Crystal backcountry on Saturday.  He found variable snow with pockets of enjoyable dust on crust in smoother terrain. Very localized pockets of soft wind slab were unreactive. Plenty of early season terrain hazards exist on solar aspects, wind scoured terrain and at lower elevations.  

Problems

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.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.