Avalanche Forecast
Regions: 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. Avoid travel on or below overhanging cornices. Watch for wet snow conditions below treeline.
Detailed Forecast
The daily dose of moderate rain and snow at rising freezing levels is expected again Friday night along with strong southerly  ridgetop winds. New storm related danger will continue Saturday, especially near and above treeline as strong southerly wind, loads lee slopes building new wind slab layers. Wind slabs will build on lee slopes, facing generally NW-NE.  Earlier formed wind slabs may still be reactive Saturday and may add to the increasingly complex snow structure, by Thursday. Large cornices should form near ridges as well, requiring travelers to avoid overhead hazard.
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, choose the terrain void of overhead hazard such as wind slabs or cornices.
Snowpack Discussion
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.Â
Fluctuating freezing levels and periods of rain or snow Tuesday through Friday have maintained about the same total snow depth at Hurricane Ridge with a few inches of new snow received each day. There have been periods of strong, mostly southerly, winds during frontal passages each day this week. Moderate rain fell Tuesday, 3/1 with rain reaching to about the near treeline band or at least 6000 feet. Â
Another front Thursday deposited about 4-6 inches of new snow at Hurricane Ridge by Friday morning, however warmer temperatures and increasing precipitation began to settle this snow by afternoon.
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
No detailed observations have been received since a week ago Friday. Since then, several storms, fluctuations in freezing levels and a mix of rain and snow, have left a variety of snow surfaces. Exposed slopes should have a strong surface crust, stripped bare of recent snow. Shaded slopes at higher elevations may still have some colder recent snow. Wind slabs and new cornices are likely near and above treeline along and below ridges, where conditions should be significantly different than mid and lower elevations. 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, 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: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind lips of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.
Cornices can never be trusted and avoiding them is necessary for safe backcountry travel. Stay well back from ridgeline areas with cornices. They often overhang the ridge edge can be triggered remotely. Avoid areas underneath cornices. Even small Cornice Fall can trigger a larger avalanche and large Cornice Fall can easily crush a human. Periods of significant temperature warm-up are times to be particularly aware.
A corniced ridgeline. A large cornice has formed at the top of the ridge. A smaller cornice has formed to the left of the trees from crossloading.
Cornices are easy to identify and are confined to lee and cross-loaded ridges, sub-ridges, and sharp convexities. They are easiest to trigger during periods of rapid growth (new snow and wind), rapid warming, and during rain-on-snow events. Cornices often catch people by surprise when they break farther back onto flatter areas than expected.
Aspects: North, North East, East, North West.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1