Avalanche Forecast
Regions: Cascades - West.
The strong storm Saturday, and subsequent additional snowfall Sunday should maintain widespread wind and storm slab layers on lee slopes near ridges Monday. Travel conservatively by staying off or below steeper slopes and avoid wind loaded terrain, especially but not limited to northwest through southeast facing terrain.
Detailed Forecast
A few isolated snow showers may linger Monday, while winds should be light and temperatures remain cool.Â
This should allow for a slowly improving avalanche danger as recent storm and wind slabs begin settling and stabilizing.
However, storm and wind slab conditions should remain sensitive or still likely to trigger in specific areas and more widespread areas near and above treeline. A variety of slopes may be wind loaded due to the local effects of terrain, however, in general wind loaded slopes should range from north to southeast facing. Â
Dangerous avalanche conditions are expected near and above tree line requiring conservative decision-making and cautious routefinding.
Be cautious with any steeper open terrain suspected of recent wind loading, leaving those more exposed features a wide margin of safety.
Travel conservatively by staying off, or below steep open slopes and avoiding the wind loaded terrain near and above treeline.
Be aware of early season hazards below treeline. The heavy rains from last week have left many creeks open at lower elevations.Â
Snowpack Discussion
Snowfall over the west slopes the first week of December ranged from 1-4 feet. An atmospheric river arrived early in the week and heavy rain fell over the west slopes, with water amounts ranging from about 5 to 8.5 inches in just 2 days ending Wednesday morning!  Since Wednesday, 15-40 inches of new snow had accumulated along the west slopes through Sunday afternoon.Â
Avalanche and Snowpack Observations
The warming and rain or heavy wet snowfall a week ago did cause avalanches and some very close calls with slides releasing on persistent weak layers above the mid-November crust. It's important to remember when looking at the snow in more protected areas  and trying to extrapolate those findings to adjacent to open avalanche prone slopes that may have avalanched recently, possibly multiple times! The snow structure of those paths may be significantly different than where you may have chosen to dig in the snow.
Persistent weak layers in the Stevens and Snoqualmie zones should have been eliminated and multiple test results this weekend from field observers have not found that layer in test results. Therefore, the persistent slab problem has been removed from the forecast problems. Â
Reports Sunday varied according to recent wind exposure during the last few days storm cycles. Multiple reports from the Skyline Ridge area near Stevens Pass, indicated relatively homogenous storm snow, well bonded to Tuesday's rain crust. No slab structure was noted in that area and good skiing was noted with some 30-50 cm or up to 2 feet of storm snow over the recent rain crust. However, across the street in the ski area, morning control produced widespread soft slab results from both explosive and ski cuts with best results on NW-SE facing terrain with slides releasing on the most recent storm interface with Friday's storm snow.
Elsewhere, from patrol at Mt Baker and Alpental Sunday, report widespread avalanches released from explosives ranging from 1-2 feet and running good distances, releasing on storm snow interfaces.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: Likely
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