Avalanche Forecast
Regions: Olympics.
Expect sensitive wind slabs on Saturday. Approach ridges cautiously and watch for firmer wind-transported snow. Storm slabs should be less reactive than Friday, but will still be possible to trigger in steeper terrain. Take a more conservative approach Saturday to enjoy the new snow safely. Early season terrain hazards still exist, such as poorly covered rocks, vegetation and creeks, particularly at lower elevations.
Detailed Forecast
Generally light and scattered showers Saturday morning should transition to more widespread shower activity in the afternoon. See the NWAC mountain weather forecast tab for more details.Â
Expect sensitive wind slabs on Saturday.  Approach ridges cautiously and watch for firmer wind-transported snow. Storm slabs should be less reactive than Friday, but will still be possible to trigger in steeper terrain. Take a more conservative approach Saturday to enjoy the new snow safely. Â
Early season terrain hazards still exist, such as poorly covered rocks, vegetation and creeks, particularly at lower elevations.
Snowpack Discussion
Warm, wet weather before Thanksgiving caused wet snow and glide avalanches as well as significant snowpack consolidation. There are no snowpack concerns below the Thanksgiving crust and in general new snow received post-Thanksgiving has reportedly bonded well throughout the Cascades. Prior to Friday at Hurricane Ridge, temperatures have hovered near the freezing mark likely leading to rapid stabilization of the new snow that fell over the course of the week.
On Friday a frontal system stalled over the Olympics and brought a fresh foot of snow with nearly steady temperatures. Winds were generally recorded in the 10-20 mph range and out of the south during this storm. Â
Observations
NPS rangers reported 5" of new snow at 8 am Friday morning along with active wind transport of the new snow.Â
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: North, North East, East, South East, West, North West.
Elevations: Alpine, Treeline.
Likelihood: Likely
Expected Size: 1 - 1
Storm Slabs
Release of a soft cohesive layer (a slab) of new snow that breaks within the storm snow or on the old snow surface. Storm-slab problems typically last between a few hours and few days. 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.
You can reduce your risk from Storm Slabs by waiting a day or two after a storm before venturing into steep terrain. Storm slabs are most dangerous on slopes with terrain traps, such as timber, gullies, over cliffs, or terrain features that make it difficult for a rider to escape off the side.
Storm slabs usually stabilize within a few days, and release at or below the trigger point. They exist throughout the terrain, and can be avoided by waiting for the storm snow to stabilize.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Possible
Expected Size: 1 - 1