Avalanche Forecast
Regions: Olympics.
Wind slabs, or storm slabs that may have formed last week should continue to stabilize Tuesday. Avoid steeper terrain features with firmer wind transported snow. Use extra caution when transitioning into potentially wind affected terrain.
Detailed Forecast
Brief high pressure should rebuild along the PNW coastal areas Tuesday. This should provide a gradual clearing trend over the Olympics, with generally light winds and cool temperatures.
This weather should allow for continued gradual settlement of any recent storm layers or wind slabs in higher exposed terrain. However, cool temperatures will help slow this process and may preserve wind slabs in higher terrain.
Watch for wind stiffened snow on a variety of aspects, including non-traditional aspects from recent northerly winds
Early season hazards still exist at lower elevations and especially around creek beds that are not filled in.
Snowpack Discussion
A weak disturbance moved across the Olympics Christmas Eve depositing 2-4 inches of new snow, with light winds recorded at Hurricane Ridge.Â
About 18 inches fell at Hurricane Ridge ending early Wednesday last week. Strong winds during this storm built unstable wind and storm slabs.
Cool and fair weather allowed this snow to mostly stabilize midweek resulting in a decreasing avalanche danger over the past several days.
In general about two feet of snow now sits on the old snow surface from a week ago.
Observations
NWAC pro observer Matt Schonwald was at Hurricane on Saturday and reported evidence of north to east winds but no wind slab or significant shear in the upper snowpack. The structure was generally F over 4F with good bonds to the Thanksgiving crust.
A nice observations Friday via the NWAC Observations page indicated about 2-3 feet of snow above the variable surfaces from early December's high pressure. Tests gave stubborn results for storm slab and there were no natural or triggered avalanches noted.
Avalanche Problems
Wind Slabs
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.
Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..
Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.
Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1