Avalanche Forecast
Regions: Snoqualmie Pass.
We have some new storm and wind avalanche concerns for Monday but give the low probability but high consequence of a deep slab avalanche the most thought before choosing more exposed terrain.
Detailed Forecast
Generally shallow new storm snow from Sunday and Sunday night is not expected to form extensive new storm slab, but may present loose avalanche concerns near terrain traps and sluff management issues in steeper terrain from Snoqualmie Pass and north.  Light amounts of new storm snow Monday afternoon may form denser but shallow storm slab over weaker snow.Â
Older wind slab formed last week may still be locally sensitive on lee slopes near and above treeline. Wind transport onto west aspects due to easterly winds near the Cascade Passes should continue Sunday night through Monday and may begin to form shallow new wind slab.   Â
Human triggered large or very large avalanches have become unlikely but are still relevant and of high consequence if able to step down to poorly bonded previous storm layers or buried persistent weak layers on top of the old January crust. Think before you jump onto an open slope in avalanche terrain where an avalanche releasing down to these depths would be deadly.Â
Cornices have grown large and may be sensitive. A cornice failure could provide a large enough natural trigger for a destructive avalanche.  Â
There's plenty of new snow to go around...continue your careful snow pack evaluation and cautious terrain selection this week.
Snowpack Discussion
Recent Northwest Weather
An extended mild and dry period occurred the latter half of January generally causing a crust to form in all areas. Very cold weather followed in early February which produced low density snowfall and faceting near and just above the crust.
Frontal systems over the weekend were weaker than the frequent systems seen over the past 2 weeks.  Until we have an extended break in the storm cycle...the running tally for water equivalent over the past 13 days is about 10-15 inches with snowfall about 8-13 feet at NWAC weather stations near and west of the crest.  An additional 6-8 inches of low density snowfall fell from about Snoqualmie Pass and north through the daylight hours Sunday.
Observations for Washington Cascades near and west of the crest
Several avalanche cycles have been seen in the last 2 weeks. Deep persistent slab remains a concern east of the Cascade crest. Be sure to read the forecast if you venture even slightly east of the crest.
The late January crust layer and associated weak layers are now deeply buried but continue to produce big results with big explosives by area ski patrol on wind loaded slopes near and above treeline. Perhaps of less relevancy to a backcountry forecast but still plenty interesting is the average 6' crown with a maximum of over 15' Alpental ski patrol was able to produce with large explosives Thursday and again on Friday in their back bowls down to the very slick January crust: Click on Alpental photos one and two.  With large explosives Crystal mountain patrol produced 4-5 ft slides produced while controlling their northside backcountry terrain Saturday and near Three Way Pk.Â
Of even greater concern to backcountry skiers and riders should be a natural wind slab avalanche that occurred near White Pass on an easterly aspect near treeline Friday morning. This natural avalanche produced an 8' crown and underscored NWAC observer Tom Curtis's report from the area Friday of heavy wind loading on lee slopes near 7000 feet (photo below).Â
NWAC Observer Dallas in the Snoqualmie Pass area Friday reported a settling and stabilizing snow pack. He saw possible 30-50 cm wind slab layers on lee slopes and storm slab that was becoming less reactive except on isolated terrain features.  He and other backcountry travelers in the Snoqualmie area over the weekend reported the facet/crust layers to be nearly 1.5 to 2 m deep.
Reports of a very large natural hard slab avalanche off steep north facing terrain of Chair Peak near Alpental partially caught 3 skiers Saturday. Luckily no on was injured in this potentially deadly avalanche with a 10' crown. This avalanche paired with the frequent and large results from ski patrol should steer the discussion to terrain management of low probability and high consequence slides that release down to old storm layers or the late Jan crust.Â
Light to moderate snowfall along with light east winds Sunday quickly re-loaded avalanche paths near Stevens Pass. DOT had to perform avalanche control several times with loose dry avalanches easily reaching the highway.Â
Pictures of a large wind slab avalanche and of large cornice growth near Gunsight Peak, White Pass, Photo by Chris Talbot, Pro Patrol 2-21-14Â
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The mid and base pack should still consist of mostly stable crusts and melt form layers from periods of warm weather earlier this winter.
Keep an eye on your riding partner in the deep snow until the new snow settles and the risk of SIS subsides.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: Possible
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
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.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 2