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Avalanche Forecast

Archived

Jan 23rd, 2019–Jan 24th, 2019

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

Snoqualmie Pass.

The Bottom Line: This recent storms deposited plenty of unstable snow, especially at higher elevations. Let these storm slabs heal, and avoid triggering avalanches, by staying off of open slopes greater than 35 degrees. If the sun comes out, snow conditions can change rapidly. Loose wet avalanches may occur from steep, sunny slopes and travel down to your location.

Snow and Avalanche Discussion

Reports from Snoqualmie Pass indicate a natural avalanche cycle occurred overnight Tuesday into Wednesday. At lower elevations rain created wet loose and slab avalanche conditions. Poor visibility Wednesday limited observations into higher terrain.

The weak snowpack structure seen near Stevens Pass and the East-Central region does not seem to be as prevalent in the Snoqualmie area--that does not mean it is absent. We were able to find buried surface hoar near Cottonwood Lake/Roaring Ridge last week. An observation from Sunday also suggests an old weak snow layer may be present. This layer could exist 1-2 feet below the snow surface. If you experience any collapsing, or see larger avalanches, it’s time to dial it back and avoid avalanche terrain nearby.

While no glide avalanches were reported, its rain events like this that bring glide avalanches to our minds. Glides avalanches can occur days after the precipitation ends and temperatures cool. If you see crevasse like features on the snow, avoid traveling on or below these slopes.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). 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.

Loose Wet

Loose Wet avalanches are the 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. 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.