Avalanche Forecast
Regions: Cascades - West.
Lingering wind slab should be the primary avalanche problem and mainly found near and above treeline Saturday. Wind slab should be less likely to trigger throughout the Cascades but look for wind loaded slopes further downslope than usual particularly in the Mt. Baker area. Also be aware of locally weak cornices in the Alpental backcountry Saturday.
Detailed Forecast
After a mostly clear start to Saturday for much of the Cascades, a fast moving frontal system will bring light snow to the north Cascades by late morning and spread south to the central and south Cascades in the afternoon. New snow amounts through 4 pm will generally be light to insignificant, but westerly winds, especially above treeline, are expected spike up by mid-day.Â
Lingering wind slab should be the primary avalanche problem and mainly found near and above treeline Saturday. Wind slab should be less likely to human trigger throughout the Cascades but look for wind loaded slopes further downslope than usual particularly in the Mt. Baker area.
Newly formed cornices have been reported sensitive in the Alpental backcountry, with one cornice fall triggering a large avalanche down to the Solstice crust Friday afternoon. Give cornices a large berth as they often break back further than expected and don't travel below slopes with large overhanging cornices.
The 12/17 PWL persistent slab problem is becoming more deeply buried and less sensitive in snowpack tests and has been removed from the avalanche problem set. Continue to identify and test this layer in snowpit tests.Â
Snowpack Discussion
Weather and Snowpack
Strong storms around the Solstice deposited generally 1 to 2 inches of water equivalent along the west slopes. A period of rain or freezing rain (Snoqualmie) during this storm cycle allowed crust layers to form in the Baker area from 4000-4500 feet, the Passes up to around 5000 feet (Stevens) to 6000 feet (Snoqualmie) and 6000-7000 feet in the Paradise area. The crust(s) were especially stout in the Snoqualmie and Paradise areas and very thin in the Crystal backcountry.Â
A strong front and strong west flow aloft was seen over the Olympics and Cascades on Monday and Tuesday. The White Pass avalanche fatality involving a skier triggered storm slab failing on the Solstice crust occurred on Tuesday afternoon. NWAC stations along the west slopes and crest had strong west winds Monday and Tuesday with 1-3 feet of new snow for the 48 hours ending Wednesday morning with a cooling trend.
A warm front kept light snow and strong winds going through much of day in the Mt. Baker area Thursday before pushing south Thursday night.  Up to 12 inches of snow fell around Mt. Baker, Stevens Pass and above 5000 feet in the Snoqualmie Pass area. Less snow was seen further at lower elevations at Snoqualmie Pass due to rain at the onset of precipitation which formed a thin breakable crust below the new storm snow. A thin rain crust was also found up to 6000 feet above Paradise Friday morning with 4" snow on top.  Â
Recent Observations
NWAC pro-observer Ian Nicholson was at Stevens Pass on Wednesday and reported no signs of instability on east slopes to 5800 feet. Ian found the Solstice crust at 65-70 cm. The 12/17 PWL was strengthening and unlikely to be triggered.  We are removing persistent slab from the set of avalanche problems as we have good confidence that the 12/17 PWL is not a reactive layer along the west slopes.Â
The rangers at Paradise reported extensive new wind slab near and above treeline Wednesday. The Solstice crust was seen at 135 cm with good bonds to the snow above.
The weather system that affected the area Thursday night generally layered new snow right side up and avalanche control results from Stevens, Alpental and Mt. Baker Friday morning only observed shallow pockets of storm slab generally in the 6-12" range. One natural avalanche likely involving the new storm snow had occurred Thursday night off the Shuskan Arm in the Baker backcountry.Â
However, at Alpental on Friday, newly formed cornices were weak with natural cornice fall observed in the afternoon. One cornice break in the Back Bowls of Alpental triggered a large slab up to 4' deep, 100' wide, 300' vertical, that broke down to the Solstice crust.Â
NWAC observer Lee Lazzara was in the Mt. Baker backcountry Friday. Lee found wind affected snow surfaces well into the below treeline band. Wind slab was stubborn on test slopes but reactive in test pits. The uneven distribution of large wind slab on varied aspects dictated more conservative terrain choices Friday. Â
NPS rangers at Paradise found the 4 inches of new snow well bonded near treeline with minimal wind slab concerns but observed ongoing wind transport of new snow on the upper volcano above 9000 ft.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, South, North West.
Elevations: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1