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RegisterMar 2nd, 2016–Mar 3rd, 2016
Olympics.
Conservative terrain selection will be essential near and above treeline as human triggered avalanches are still likely. Choose moderately angled terrain and avoid wind loaded slopes, saving those steeper lines for another day.
A period of moderate rain and snow at rising freezing levels is expected Wednesday night along with strong S-SW ridgetop winds. Showers should taper quickly Thursday morning. A modest cooling trend is expected by early Thursday, however, the new storm related danger will continue through Thursday due to strong southwest winds loading lee slopes during showers Wednesday night.
Storm slab instabilities should be stabilizing, but may still be sensitive Thursday. Wind slabs will continue to build Wednesday night on lee slopes, facing generally NW-NE. Earlier formed wind slabs may still be reactive Thursday and may add to the increasingly complex snow structure, by Thursday.
Conservative terrain selection will be essential near and above treeline to avoid wind loaded terrain and features. Choose moderately angled terrain and avoid wind loaded slopes, saving those steeper lines for another day.
Weather and Snowpack
Very mild weather a week ago allowed for the formation of a strong melt-freeze crust.
The last significant snowfall in the Olympics occurred Sunday, 2/28 through early Monday when about 12 inches of snow accumulated at Hurricane Ridge accompanied by a cooling trend. Moderate S-SW winds transported snow to lee slopes Sunday and Sunday night.
Fluctuating freezing levels Tuesday and light precipitation caused some rain or light snow at times through Tuesday with strong southerly winds.
The mid and lower snow pack along the west slopes should generally be a stable mix of crusts and layers of moist and rounded snow crystals.
Recent Observations
NWAC pro-observer Matt Schonwald was at Hurricane Ridge Friday and found mostly consolidated stable snow. N to E slopes had areas of 25-30 cm of wind transported 4F snow well bonded to 1F melt form grains in the upper snow pack. South through west slopes were melted out in some places with shallower dense stable snow in others.
No recent observations are available for the Olympics, but rainfall on Tuesday likely caused a natural avalanche cycle.