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Avalanche Forecast

Archived

Jan 18th, 2019–Jan 19th, 2019

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

Regions

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The Bottom Line: A strong storm will impact the West-Central zone Friday night and Saturday adding more snow/ rain to the area and keeping the avalanche danger elevated. Be patient Saturday. Stay off of open slopes greater than 35 degrees where you can trigger avalanches within the new snow.

Snow and Avalanche Discussion

Another round of heavy precipitation Friday night into Saturday will only serve to add more load to the snowpack and keep the avalanche hazard elevated. The avalanche danger will likely peak overnight Friday/Saturday as the heaviest and warmest precipitation impacts the area. However, heavy snow showers and moderate winds may cause very dangerous avalanche conditions to linger into the daylight hours. As the weather cools, and the snow showers decrease, avalanche danger will slowly decline, but if you find yourself in areas of sustained heavier snow showers, expect that the avalanche danger may locally maintain or increase.

We received reports of natural, human-triggered, and explosive triggered avalanches from the Mt Baker area Friday and given similar recent weather impacts, we suspect that the Mountain Loop may behave similarly. At least one of these avalanches released after several people traveled on the same slope. Avalanches occurred on W-N-NE aspects above 4800 ft, where mostly cold dry snow accumulated. A subtle weakness found between Thursday and Friday’s storm snow seemed to be the culprit in most of these events. We expect similar weaknesses within the storm snow again Saturday in the Mountain Loop.

Problems

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.

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.