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Avalanche Forecast

Archived

Mar 30th, 2015–Mar 31st, 2015

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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Moderate danger does not mean it's OK to let your guard down. Increasingly sensitive avalanche conditions involving generally shallow amounts of new snow are likely on lee slopes near and above treeline as well as loose wet avalanche concerns during sunbreaks and daytime warming Tuesday afternoon. Intense showers may produce unstable graupel layers for future snow to fail on. 

Detailed Forecast

A frontal system passing through late Monday night should be followed by orographic showers and a cooling trend Tuesday. Showers may be locally intense Tuesday afternoon with more moderate snowfall accumulations possible near a Puget Sound convergence zone between Stevens and Snoqualmie Passes. 

Moderate danger does not mean it's OK to let your guard down. Increasingly sensitive avalanche conditions involving generally shallow amounts of new snow are likely on lee slopes near and above treeline as well as loose wet avalanche concerns during sunbreaks and daytime warming Tuesday afternoon. Intense showers may produce unstable graupel layers for future snow to fail on.      

Cornices won't be listed as an avalanche problem but be aware of new cornice growth along ridgelines.

Snowpack problems west of the crest for the time being should be in the upper or surface layers. The mid and lower snowpack west of the crest consists of layers of stable consolidated rounded grains or melt forms and crusts from multiple warm periods this winter. Many areas at the lowest elevations do not have enough snow to cause an avalanche danger.

Snowpack Discussion

Winter made a bit of a comeback in the Northwest in mid to late March. Several storms brought heavy snow to the near and above treeline areas west of the crest, especially on the volcanoes. 

After a period of natural and skier triggered loose avalanches last Tuesday, a warm front brought moderate to heavy rain Wednesday through Thursday morning. This caused an avalanche cycle and snowpack consolidation west of the crest with many large natural avalanches observed in the Mt Rainier area above treeline.

A vigorous front and short wave crossed the Northwest Friday night causing strong west-southwest winds along with some rain and snow. Snow levels lowered enough by Saturday to produce 2-3 inches of snowfall at higher NWAC stations west of the crest. The new snow had bonded well to the moist surface on a windloaded ENE aspect near treeline in the White Pass backcountry. 

Mt. Baker picked up another inch of water Sunday and Sunday night with snow levels 5-6000 ft, while other locations experienced fair weather. Warm weather Monday lead to further settlement at the higher NWAC stations.  

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.

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.