Avalanche Forecast
Regions: Olympics.
Take time to identify features where wind loading has occurred and go around them and watch for sun effects on steep solar slopes.
Detailed Forecast
Fair weather should be seen Monday with a slight warming trend.
Previous mostly small wind slab may linger mainly on lee northwest to southeast slopes. Watch for signs of firmer, hollow wind transported snow.
Some sun and warmer temperatures should make loose wet avalanches possible on steep solar slopes. Watch for wet surface snow deeper than a few inches on solar slopes and roller balls that usually precede loose wet avalanches.
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Snowpack Discussion
A warm front last Thursday caused heavy rain in the Olympics and this caused a loose wet avalanche cycle on steep slopes in all the elevation bands.
This was followed by cooler weather and some snow. The cooling formed good bonding to the forming crust as observed by NWAC pro-observer Matt Schonwald Friday.
Matt reported generally stable surface snow conditions with no layers of concern in the BTL and NTL elevation zones. Overall the snowpack consisted of a few inches of saturated snow, well bonded to supportive dryer, old snow and a newly forming crust. Stability tests were all negative. Some transport of loose surface snow was seen being deposited on the northerly facing terrain below ridges, but no distinctive wind slab had formed as of Friday afternoon.Â
Hurricane Ridge weather station: NWAC forecaster Garth Ferber was at Hurricane Ridge Thursday and with the help of NPS IT staff our weather station is back online!  We appreciate everyone's patience and believe that our new internet connection to the weather station will prove to be far more reliable than the aging microwave it replaced last spring.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, North West.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1
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.
Aspects: South East, South, South West.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1