Register
Get forecast notifications
Create an account to receive email notifications when forecasts are published.
Login
Archived

Avalanche Forecast

Feb 25th, 2014–Feb 26th, 2014
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
3: Considerable
The avalanche danger rating at treeline will be considerable
Below Treeline
3: Considerable
The avalanche danger rating below treeline will be considerable
Alpine
3: Considerable
The avalanche danger rating in the alpine will be considerable
Treeline
2: Moderate
The avalanche danger rating at treeline will be moderate
Below Treeline
2: Moderate
The avalanche danger rating below treeline will be moderate

Regions: Stevens Pass.

We have a variety of avalanche concerns Wednesday depending upon terrain choices, ranging from loose-wet slides away from the passes near treeline and below, large cornices near ridges, some new storm and wind slab,  and finally the remaining threat of deep persistent slabs involving the late January crust layers, although these remain a low probability but high consequence.  Professional observers choosing not to travel in large exposed terrain given this possibility and this seems prudent for all back country travelers until we have confidence that threat is eliminated.   

Review this extract regarding deep persistent slabs from this excellent book:   

Detailed Forecast

Skies should remain relatively clear Wednesday with continued warm temperatures. Freezing levels are expected to remain at about 8000 ft Wednesday and along with sunshine should maintain wet snow conditions with a likelihood of triggered loose-wet avalanches near and below treeline.  Above tree-line areas should expect weakening cornices along ridges and possible older wind slab on open lee slopes. These conditions will warrant careful travel and terrain choices. 

Watch for wet surface snow conditions and given the deep recent storm snow, expect any wet-loose avalanches that start small to possibly entrain large amounts of snow.  Avoid terrain traps and steep slopes and watch for signs of natural wet loose activity.   

Cornices have grown large over the last 2 weeks. A cornice failure could provide a large enough load to trigger a destructive avalanche. With the warming again Wednesday...expect cornices to become more sensitive and likely to fail.  

Continue your careful snow pack evaluation and cautious terrain selections during the work week.

Snowpack Discussion

Recent Northwest Weather

An extended mild and dry period occurred the latter half of January generally forming a crust in all areas. Very cold weather followed in early February which produced light low density snowfall, near surface faceting, and faceting near and just above the crust.

Weaker frontal systems last weekend followed the frequent strong storms over the past 2 weeks.  We have finely ended the extended storm cycle as of Monday night, capping off impressive amounts of some 8-15 feet of new snow with a mixture of rain, snow and some freezing rain in the passes.  

Skies have cleared Tuesday with a mix of sun and clouds with temperatures climbing well above freezing with many afternoon temperatures in the lower 40's at NWAC stations away from the passes.  This current warm conditions and rain have drastically changed the snowpack conditions from recent deep powder snow to wet snow conditions. 

Observations for Washington Cascades near and west of the crest

Several avalanche cycles have been seen in the last 2 weeks, including an active avalanche cycle in the Mt Baker backcountry on Tuesday due to rapid warming and solar affects on recent storm snow.  Several triggered and natural slab avalanches released on Tuesday on a variety of elevations and aspects with some cornice induced or loose-wet avalanche triggered slab releases as well.  One very large deep slab released on the SE aspect of Goat Mountain that likely released down to the early February facet/crust critical layer as the crown was estimated at 6-8 ft.  That slide released between 11 am and noon when solar effects were maximized. While the deep persistent slab remains a major concern east of the Cascade crest, it is also evident along the west slopes as well.  These deep weak layers are unlikely to release by the weight of a skier and likely need a much larger trigger, however as this slide shows, a collapsing cornice, warming and sunshine all contributed to tip that balance.  The best way to deal with these conditions remains avoiding large open terrain, as inviting as it looks.  These slides could also possibly be human triggered at a thinner spot in the slab such as near rocky outcrop or a micro terrain feature.  

 

Natural deep slab release (center left) on SE flank of Goat Mtn 2/25 est.crown 6-8 ft.plus numerous fresh loose-wet slides. image Patrick Kennedy

Skier triggered slab on Table Mtn, Tuesday 2/25, fortunately uninjured. Photo, Patrick Kennedy

More natural loose and slab releases on Mt Herman near Mt Baker, Tuesday 2/25. Patrick Kennedy

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 north-back terrain Saturday and near Three Way Pk. While unlikely to produce a human triggered slide on these deeper weaknesses, it becomes more possible if a larger trigger is involved, such as a large cornice collapse initiating a slide that may break down to this persistent layer.

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.  It is believed this slide was initiated by a smaller slide or possible cornice failure then stepped down to the deep layer. 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. 

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. 

Avalanche Problems

Deep Persistent Slabs

Release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer, deep in the snowpack or near the ground. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage. They commonly develop when Persistent Slabs become more deeply buried over time.

 

Deep Persistent Slabs avalanches can be destructive and deadly events that can take months to stabilize. You can trigger them from well down in the avalanche path, and after dozens of tracks have crossed the slope.

 

A snowboarder triggered this Deep Persistent Slab near treeline, well down in the path.

Deep, persistent slabs are destructive and deadly events that can take months to stabilize. You can triggered them from well down in the avalanche path, and after dozens of tracks have crossed the slope. Give yourself a wide safety buffer to handle the uncertainty, potentially for the remainder of the season.

Aspects: All aspects.

Elevations: All elevations.

Likelihood: Possible

Expected Size: 1 - 2

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: East, South East, South, South West, West.

Elevations: All elevations.

Likelihood: Likely

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, West, North West.

Elevations: Alpine, Treeline.

Likelihood: Possible

Expected Size: 1 - 2