Avalanche Forecast
Regions: Cascades - North West.
2-3 ft of fresh snow and wind maintains dangerous avalanche conditions at upper elevations. At mid-elevations, danger may lurk where the snow sits on a smooth crust or where wind transport has consolidated the snow into a slab. Ease into your backcountry season with conservative terrain choices, giving the storm snow time adjust to the loading.
Discussion
On Thursday afternoon, a backcountry traveler in this zone triggered a slab avalanche in near treeline terrain, propagating 30 ft wide and running 500 ft of vertical as reported here.
Uncertainty remains higher than normal as we exit the first significant storm cycle of the season. Combining a significant instability observation with a general lack of recent observations beyond the Mt. Baker ski area / Austin Pass areas, we have significant uncertainty for tomorrow's forecast. We think that higher elevations received enough new snow and wind that slabs lurk and conditions are dangerous. We are fairly confident that terrain anchors readily visible under the snow surface will suppress avalanche activity below treeline. However, in the near treeline terrain, Mt. Baker Pro Patrol reported 2-3 ft of unconsolidated new snow that fell over a 3-day period. Above approximately 5000 ft, that new snow sits on an old snow interface. We don't know whether there are places where the bonding to the underlying bed surface may be poor or where winds/solar inputs have helped to consolidate some of this new snow into a slab. This uncertainty motivates an assessment mindset.
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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
While we don't have direct observations above treeline, there's been enough snow and wind that we think you can easily trigger a large avalanche on any terrain steeper than 35 degrees. Near treeline, Mt. Baker's 2-3 ft of recent snowfall needs time to settle. and we all need time to assess the conditions, so ease into the terrain. Above 5000 ft, we have a bed surface (old snow) and we think that on specific terrain you will find a slab. Utilize small test slopes that might show signs of instability. Cracking, shooting cracks, and collapsing are all signs that you have unstable snow nearby. Dig frequently to the old/new snow interface with each aspect change or as you go higher in elevation. If you find stiff or slabby snow, a weak interface, or evidence of slab avalanche activity, you should dial back your terrain, choosing only supported slopes less than 35 degrees.
As the weather gradually clears, look upward for solar inputs on Saturday, and beware of rollerball activity leading to shallow loose wet avalanches on southerly slopes.
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: Alpine, Treeline.
Likelihood: Likely
Expected Size: 1 - 1