Avalanche Forecast
Regions: Olympics.
New snow at higher elevations or rain amounts and solar effects are hard to predict on Wednesday. Remember to evaluate snow and terrain carefully on Wednesday.
Detailed Forecast
A weakening upper low from the Gulf of Alaska will move to the Northwest on Wednesday. The main rain or snow should be over Oregon. In the Olympics and Washington Cascades this should cause mostly light showers and cool temperatures. Some consolidation and cooler temperatures should slightly lower the avalanche danger from Tuesday to Wednesday. But new snow at higher elevations or rain amounts and solar effects are hard to predict on Wednesday. Remember to evaluate snow and terrain carefully on Wednesday.
Any additional rain or snow and late March solar effects should make wet snow conditions and wet loose avalanches possible mainly near and below treeline on Wednesday. Watch for wet surface snow deeper than a few inches, roller balls in surface snow and small natural wet loose releases that usually precede more major wet loose snow avalanches.
New or recent small areas of wind slab should also be possible Wednesday mainly above treeline on lee slopes. Watch for signs of cracking or firmer wind transported snow.
Snowpack Discussion
A cold front crossed the Northwest Wednesday last week. This system produced more snow in the Cascades with the Hurricane Ridge weather station recording only about 4 inches of new snow at low temperatures and with generally light winds. On Friday afternoon NWAC observer Katy Reid denser wind slab on N thru SE near treeline that was stubborn in stability tests and did not note in any recent avalanches.
Warmer weather with increasing sun was seen Saturday to Monday. On Sunday Katy reported numerous small to large wet loose avalanches on solar aspects but dry loose avalanches on due north aspects at higher elevations.  She also found wind slab in the limited above treeline zone near Hurricane Ridge to be prone to snow pit test failures down 20 cm at a melt freeze crust on the colder N-NE aspects.
A front is crossing the Northwest on Tuesday causing mostly light to locally moderate rain and snow. In the Cascades NWAC observer Dallas Glass at Snoqualmie reports wet snow conditions, roller balls and a small triggered wet loose avalanche. The Mt Baker and Alpental patrols report softening surface crusts over wet snow.
Avalanche Problems
Loose Wet
Release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. They generally move slowly, but can contain enough mass to cause significant damage to trees, cars or buildings. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
Travel when the snow surface is colder and stronger. Plan your trips to avoid crossing on or under very steep slopes in the afternoon. Move to colder, shadier slopes once the snow surface turns slushly. Avoid steep, sunlit slopes above terrain traps, cliffs areas and long sustained steep pitches.
Several loose wet avalanches, and lots of pinwheels and roller balls.
Loose wet avalanches occur where water is running through the snowpack, and release at or below the trigger point. Avoid terrain traps such as cliffs, gullies, or tree wells. Exit avalanche terrain when you see pinwheels, roller balls, a slushy surface, or during rain-on-snow events.
Elevations: Treeline, Below Treeline.
Likelihood: Possible
Expected Size: 1 - 1
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.
Likelihood: Possible
Expected Size: 1 - 1