Avalanche Forecast
Regions: Snoqualmie Pass.
Shallow storm slabs are possible Sunday afternoon. Watch for new snow that bonds poorly to existing surface crusts or in areas of preserved surface hoar.
Detailed Forecast
Generally very light precipitation is expected Sunday morning, with light to moderate rain and snow in the afternoon along the west slopes. Â The Cascade Passes will locally stay cooler through Sunday afternoon thanks to cool easterly flow. A frontal passage is expected later Sunday afternoon, switching the Pass winds to westerly and popping snow levels up to free-air levels of 5000 ft.
New snow may bond poorly to surface crusts, allowing shallow storm slabs to develop Sunday afternoon especially on lee aspects near and above treeline. New storm slabs may also fail on surface hoar that survives on shaded aspects generally below treeline. Â Â
A fair amount of uncertainty surrounds a potentially stronger frontal system Monday but generally expect increasing avalanche danger Monday.Â
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Snowpack Discussion
Last weekend (Jan 24-25th) a warm and wet weather system caused high snow levels and rain. Most NWAC sites west of the crest had about 1-3 inches of rain. This caused loose wet avalanches, some possible wet slab avalanches and consolidation.
This week, high pressure aloft has caused abundant sunshine and mild temperatures, generally well into the 40's and at times lower 50's.
The snowpack is therefore dominated by strong surface crusts, limiting the avalanche potential. There has been some surface hoar growth over the past few clear nights and this may be preserved on shaded terrain and mainly found below about 5000 feet, and especially at lower elevations where more fog or low clouds have formed. See Jeff's video from the Steven's Pass area below.
The snowpack west of the crest should mainly consist of stable consolidated rounded grains or melt forms and crusts from multiple warm periods this winter.
Avalanche Problems
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