Avalanche Forecast
Regions: Cascades - South West.
Uncertainty and avalanche danger exists as a result of the season’s first major storm. Temper your excitement, be conservative with your terrain choices, and ease into winter. Early season hazards persist despite the new snow.
Discussion
Paradise and White Pass both picked up over 2.00â of water during the storm, while Crystal received over 1.00â, respectfully. Throughout the zone, storm snow now sits atop a variable early season snowpack, including rotten snow near the ground in isolated locations.Â
Recent observations have been limited to the Crystal area. Jeremy Allyn toured to Crown Point today and reported multiple collapses and observed two recent avalanches. Additionally, Crystal Mountain Ski Patrol saw Gazex results start as loose dry avalanches before triggering slabs further off the ridge. These red-flag results, along with numerous small avalanches reported in the Paradise area prior to the storm, should be taken into consideration throughout the zone. Check out The Regional Synopsis for more information on these layers.
Dry Loose and Slab activity at Crystal Mountain. Photo: Mike Haft (12/13/2019)
Snowpack Discussion
December 12, 2019
After a dry November, this week marks the beginning of more winterlike weather across the region with snow at middle and pass level elevations. While thereâs uncertainty in the weather forecast, it does appear that the snowpack will continue to build to some extent over the coming week.Â
Throughout much of the region, the slow start to winter has left avalanche conditions distinctly defined by elevation. Slopes above 5,500-6,000ft hold a layered snowpack that provides enough coverage for winter travel and avalanches. Below this elevation, most slopes were bare until the past week. At these lower elevations, it will likely take another round of storms before larger avalanches are possible and travel becomes easier.
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Image courtesy of the Natural Resources Conservation Services interactive map showing Snotel weather stations measuring well below normal snow water equivalent for this season so far.
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Upper Elevations
The lack of significant snowfall has resulted in commonalities throughout the region. Slopes above about 5,500ft currently hold the âdeepestâ snow cover and the most layered snowpack. Until the lower elevation terrain builds a more substantial snowpack, the upper elevations will hold the most potential for producing large avalanches. If you dig into the snow in these areas, youâll find a range of height of snow and a variety of layers. Here are a few layers to note:
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The interface of older snow and any new incoming snow would be the first interface to check.
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Snowfall around December 7th and 11th may have buried surface hoar and near-surface facets in some locations. As of Dec 12th, these interfaces can be found 1-2â below the surface.
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A layer of facets can be found near the middle of the snowpack, buried just before Thanksgiving. Where found, the facets are often rounded or have even undergone some melt-freeze metamorphism from liquid water.
While these layers give you something to look at in snow profiles, they may not be your main snowpack concern for the day. Continue to check the daily zone forecasts for the most up to date avalanche conditions. Weâll monitor these layers as future weather brings changes to the snow and avalanche conditions.
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A layer of facets in the middle of the snowpack resulted in sudden test results on Dec 11th. Rock Mtn, N, 6270ft. Photo: Josh Hirshberg.
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Middle and Lower Elevations
At most locations below 5,500ft, slopes are still building uniform snow cover. In many zones, the hazard of hitting rocks or shallowly buried objects may be more significant than the avalanche danger. Depending on future weather, the snowpack could continue to form or could, unfortunately, melt out to the ground. While thereâs little layering of note at these elevations, avalanches arenât completely out of the question with the right weather input. Further low elevation snowfall or warming could drive avalanche activity. The East North forecast zone, including Washington Pass, has more low elevation snow than other zones and therefore more potential for avalanches at these elevations. As with the upper elevations, weâll wait and see what the next round of weather brings.
Avalanche Problems
Storm Slabs
Heavy snowfall likely formed storm slabs on all aspects at middle and upper elevations. Wind drifting can increase the depth of a storm slab. The new snow may not have bonded well to old snow surfaces, and mid-storm layers may be problematic as well. Be conservative and ease into terrain by starting with small test slopes and evaluating what is happening with the snow. Watch for shooting cracks, collapses, and recent avalanches. Avoid traveling on slopes greater than 35 degrees when you find strong snow over weak snow, and steer clear of big terrain features like large bowls and chutes. Expect to encounter shallowly buried objects and challenging travel conditions, especially at lower elevations.
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: Likely
Expected Size: 1 - 1