Avalanche Forecast
Regions: Snoqualmie Pass.
Very dangerous avalanche conditions are expected with many large to very large natural avalanches likely. Some of these slides may become destructive in force and as a result, travel in avalanche terrain is not recommended.
Detailed Forecast
New snowfall received over the past week, and especially the most recent snowfall from Saturday night and Sunday, may quickly become unstable with strong sunshine and warming expected Tuesday.  The recent snowfall will be very susceptible to strong spring solar effects and rapid warming Tuesday.  This expected weather following closely after such heavy recent spring snow storms, should lead to a significant avalanche cycle and a generally high avalanche danger in most areas, especially direct sun exposed terrain.
Natural or triggered avalanches should be likely to very likely Tuesday and travel in avalanche terrain is not recommended. Â Some of these slides may become large and potentially destructive in force. Â Expect very dangerous avalanche conditions.
These expected very dangerous avalanche conditions are likely to persist through the week with the warmest weather of the season expected Wednesday and Thursday.Â
Snowpack Discussion
The last full week of April has felt more like winter than spring; the Forks, WA freezing level has averaged 4000 feet over the last week which is more than a 1000 feet lower than the average for the entire month of March. Upper NWAC stations at several sites have now reached their season maximum snowdepths, including: Green Valley, Crystal Mt, Paradise, MRNP, Pigtail Peak, White Pass, and Timberline, Mt. Hood.  Many other sites have neared their season maximums reached in late March. Â
Water equivalents at NWAC stations near and west of the crest over the past two days ending Monday morning are generally near the 1 inch range, with between  2.5-4.5 inches over the past week.  Snowfall received during this time near treeline zone is in the 1.5-3 foot range with more snow expected at higher elevations. Â
Most west slope areas received about 1 foot of new snow since Sunday.  This most recent snowfall, in addition to last week's snow, should be readily available to become involved in avalanches with the expected warming over the next several days.
In addition to the most recent new snow, WSDOT field observations on Chinook Pass, indicate that significant old wet snow is now becoming entrained in avalanches initiated in the most recent new snow.  This has led to some very large and dangerous avalanches, both last week and as recent as Monday, April 28th.  Â
Avalanche observations (note that we receive far less observations than during winter):
Mt. Baker:  On Friday near Church Mtn, Brian Kennedy reported small wet loose slides on solar aspects becoming more reactive in the afternoon with sunbreaks and warming with a few point releases stepping down and entraining soft slabs about 20" (50 cm) down, but not propagating.Â
Snoqualmie Pass: A triggered slab avalanche Sunday, caught, carried and severely injured a skier in a steep chute on Snoqualmie Mountain, requiring a long and arduous rescue.
Alpental: The Alpental ski patrol reported a widespread natural avalanche cycle Wednesday night, followed by easy ski triggering in the above and near treeline zone Thursday producing 8-12" storm slabs. Large wet loose avalanches were easily ski triggered below treeline Thursday.  With explosives Friday, Alpental patrol produced loose slides that entrained and ran further than the Wed night natural cycle. Ski cuts Friday produced isolated soft slabs.Â
Chinook Pass: On Thursday morning the DOT crew reported a large wet loose avalanche that reached the road entraining 12-16" of new storm snow.  Later Thursday, during extended sun breaks, a large natural avalanche buried a bulldozer, and the operator inside, for several hours before avalanche crews could perform additional control work before rescuing the trapped worker (see photo1 and photo2 by John Stimberis, WSDOT).   Â
Tatoosh Range, MRNP: On Saturday, NWAC Observer Dallas Glass found shallow but hard wind slab that was easily ski triggered on a N aspect above treeline (see below). Dallas also found widespread evidence of point releases from earlier in the week that had stepped down to lingering slab instabilities. Highlighting the power of late April insolation during this cool week, check out this picture from Dallas of a glide avalanche on a SW aspect at 5000'; the new snow from this week released on a lubricated smooth rock surface.  Dallas reported additional snowfall Sunday was producing more storm and wind slab concerns in all elevation bands. Â
D1-R1-HS-ASi-N, Tatoosh Range, Dallas Glass 4-26-14
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.
Aspects: East, South East, South, South West, West.
Elevations: All elevations.
Likelihood: Very Likely
Expected Size: 1 - 2
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: 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.
Elevations: Alpine, Treeline.
Likelihood: Likely
Expected Size: 1 - 1