Avalanche Forecast
Regions: Stevens Pass.
Bottom Line: Cooling should help new snow profiles, however strong ridgetop winds should continue to build larger wind slab on many lee slopes exposed to wind. The most dangerous slopes should be steep NW-SE facing slopes below wind exposed ridges, mainly near and above treeline.Look for increasing avalanche danger later in the day especially on wind loaded slopes in the near and above treeline areas zones.
Detailed Forecast
A moderate to strong frontal passage will move across the area Wednesday evening bringing a period of moderate to heavy precipitation through the evening then cooling a shift to moderate showers along the west slopes. The strong westerly flow should maintain showers along the west slope areas and over the volcanic peaks through Thursday morning at further cooling. This storm should build unstable wind slab layers on many lee slopes near ridges ranging from NW through SE aspects.  The cooling trend by Thursday should help with the new snow profile and limit storm slabs sensitivities but keep an eye for layering using a variety of quick probes and hand shears within the new snow. Â
Crest level winds should remain strong overnight Wednesday through much of Thursday which will continue to transport falling snow as well as earlier deposited snow thus continuing to build unstable wind slab as well as some cornices.Â
Less snow and lighter winds as well as continued low snow depths should not appreciably increase the danger at lower elevations.Â
Another front should begin spreading renewed precipitation over the area late Thursday afternoon or evening to again lead to an increasing danger, but mainly after dark Thursday.Â
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Snowpack Discussion
The last significant storm crossed the area last Thursday, initially producing rain or wet snow before transitioning to snow at lower elevations. New snow amounts varied from north to south and with elevation. Upper elevations in the north received about 20-30 cm (8-12 inches) of new snow with lower elevations and areas in the south getting about 10-20 cm (4-8 inches).
Sunny weather with increasingly warm temperatures were experienced over the weekend and produced some small loose wet slides on solar aspects. Less warming was seen in the passes due to cooler easterly flow.Â
Generally good bonding was seen from the last storm snow to crust interface, however some exceptions occurred, such as a few sensitive storm and wind slab releases last Saturday in at least 2 different human triggered incidents. A climber triggered 2 separate slides and was caught in a 1 foot storm or wind slab in the east facing bowl below Chair Peak near Snoqualmie Pass at about 5500'.  The climber was not seriously injured.
A skier also triggered but was not caught by a 1-1.5 foot storm or wind slab on a south facing slope on Mt Herman near the Mt Baker ski area at about 5700 feet. The bonds here may not have been as good between the recent and old snow with the old crusted snow acting as a bed surface. Sunshine may have helped to activate this slope.
Surface hoar formed with clear cool nights this weekend in the lower elevations of the cooler Cascade passes and on shaded aspects throughout the west slopes. This surface layer should have been destroyed by the warming temperatures Monday night and Tuesday along with rain at lower elevations and freezing rain/mixed precipitation in the passes.  Generally light amounts of new snow at mid and higher elevations received Tuesday and Tuesday night should have bonded well to the old snow surface.
A stronger storm moving into the region Wednesday is beginning to add additional load to the upper snowpack as well as build new unstable wind slab layers on many lee aspects ranging from NW-SE.
There should be less danger increases in areas that received less recent storm snow snow such as Hurricane Ridge and Crystal Mountain, however heavier precipitation expected overnight Wednesday should quickly change that.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.
Elevations: Alpine, Treeline.
Likelihood: Likely
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, South East, North West.
Elevations: Alpine.
Likelihood: Possible
Expected Size: 1 - 1