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Avalanche Forecast

Archived

Mar 10th, 2014–Mar 11th, 2014

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

Regions

Snoqualmie Pass.

Increasing avalanche danger is expected Tuesday, especially during the afternoon on steeper slopes receiving direct sun and in areas where more recent new snow has accumulated.

Detailed Forecast

Light rain or snow showers should end Monday night with skies clearing.  Tuesday should be mostly sunny and start cool but warm rapidly, especially by midday and afternoon. 

The cooling through Tuesday morning should allow for shallow new crust formation near or at the surface helping to temporarily limit wet snow avalanches early Tuesday.  However, the near spring sun angles are gaining power and combined with rising freezing levels later Tuesday should increase the possibility of triggered wet loose avalanches especially on direct sun exposed slopes near and below treeline. Watch for pinwheels and surface wet snow deeper than a few inches.

Areas of new wind slab are possible above treeline at higher elevations, watch for signs of wind transported snow.

While the likelihood or triggering a wet slab on a deeper layer is unlikely, this will be a continued concern moving forward into the spring, especially in areas that have received significant recent rain, allowing water to penetrate to these deeper weak layers from mid-winter. 

Snowpack Discussion

The past month has had 2 major storm cycles producing widespread avalanche cycles in the Cascades.

The first two week storm cycle ended February 25th and deposited about 7-12 feet of mostly wet heavy snow at most sites near and west of the crest and caused numerous storm avalanches.

The latest storm cycle wound down this past Sunday morning producing similar water equivalents as the February cycle.  Water equivalents and snowfall for the past week are about 9-13 inches and 2-6 feet at NWAC sites.  This produced many avalanches this past week including reports from Holden Village, Stevens Pass, Tumwater Canyon, Alpental and Snoqualmie with pass closures at times last week.

Wet loose avalanche on 5 March on Spiral Butte at White Pass. Photo John Stimberis/WSDOT.

The latest front moved across the area on Sunday morning and a few more avalanches were seen in some areas. The Mt Baker ski patrol reported 2 explosively triggered large wet loose avalanches that destroyed trees but nothing human triggered. The Alpental ski patrol Snoqualmie DOT reported saturated surface snow layers but limited effects from all the rain Saturday night. A snow cat triggered a large wet loose avalanche at White Pass on Sunday morning at 5000 feet.

Looking down on a snow cat triggered large avalanche at White Pass on Sunday morning 9 March. Photo by Chris Talbot/White Pass Ski Area.

The ski patrol at Crystal Mountain both Sunday and again Monday morning produced deep wet slab releases with large explosive charges.  The slides are releasing to deep layers from early this winter. These slides were generally on east to northeast slopes at about 6000-6800 feet with crowns of 4 to 6 feet and up to 10 feet in spots with some trees destroyed.  The slide released Monday was a wet slab following more rainfall and propagated across a wide bowl.  While it is unlikely these deep slides could be human triggered, it remains a possibility, especially if initiated by a thin spot in the slab such as near rocks or trees.  As liquid water has now penetrated to deep in the snowpack in places that have received significant recent rain these concerns should remain with us into the spring, especially during times of rain or extended warm periods.  It may also be possible to initiate a wet slab release as a result of loose wet slides triggering a deeper layer.  As a result of this recent activity, wet slab avalanches will now be listed as a concern near and west of the crest. These avalanches may continue to release at the January crust and faceted layers from early February.  We will continue to track these layers as we move into the spring.  Here is a link to more information about wet slabs.

Problems

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.

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.

Wet Slabs

Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.