Avalanche Forecast
Regions: Snoqualmie Pass.
Recent winds wreaked havoc on the snowpack around the Snoqualmie area, blowing snow into firmer and thicker slabs at all elevations. Take time to identify and avoid steep slopes where you suspect the wind deposited snow. Avalanches may trigger more easily and grow larger as you ascend towards the tops of prominent peaks.
Discussion
The storm has ended, things are quieting down, and the avalanche danger is slowly dropping. Most areas picked up around 12-15â of snow Sunday and Monday. Very few avalanches were reported during this cycle, however, stormy conditions limited observations and travel. Some lingering uncertainty still exists with the current snowpack. Snow profiles on Sunday and Monday identified small sugary facets around the 2/22 interface below the recent snow. The exact location of these weak grains is very difficult to define. Observations suggest they could be most prevalent on W-N-E aspects in locations east of the Hyak exit or above 5000â in the Alpental Valley. When we have uncertainty with persistent grains, it can be a good time to choose lower angle and lower consequence terrain until more information is known.
Snow profile highlights the 2/22 and 2/13 crust in the snowpack. W 4800â Kendall Peak Photo: Dallas Glass
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Snowpack Discussion
February 20, 2020 (The regional synopsis is updated every Thursday @ 6 pm)
Intermittent Storms
Januaryâs non-stop pattern of storms extended into the first week of February. Since then, weâve transitioned to more intermittent storms with notable stretches of high pressure and dry weather. We now see more variability through the region in the snowpack layering and avalanche conditions than in January.Â
Significant periods of calm weather in February have allowed avalanche danger to decrease between storms. During the clear periods, strengthening late winter sun and gradual warming has brought some loose wet avalanche cycles to sunny slopes. Even so, from February 1st-20th there were 10 days when one or more zones were forecasted at all Low danger. In comparison, the month of January had zero days with any zone forecasted at all Low avalanche danger.Â
Surface hoar near Snoqualmie Pass. February 19th. Photo: Ely Gerbin
Looking Forward
As we look forward, there are a number of considerations that are pertinent to most zones. The pattern of storms separated by clear periods may form new weak layers and interfaces to monitor. Many zones hold variable surfaces that warrant consideration as a travel hazard. In the Mt Hood Meadows area, two fatalities were related to falls on slick surfaces over Presidentâs Day weekend. Another important consideration is the cornice growth that occurred in the past month from predominantly west winds. Very large cornices loom on ridges in most zones, except for possibly the Olympic Mountains. Future warming could be the added ingredient needed for cornices to fall. A close call with a cornice-triggered avalanche near White Pass on February 12th is a reminder of the potential hazard that cornices can pose.Â
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A party of three triggered this avalanche from below on a southeast aspect at 5400ft near Skyline Lake, Stevens Pass on February 16th. Two members of the party were fully buried and one was partially buried. The party self-rescued and no injuries were sustained. Photo: Dustin RiggsÂ
Weak Layers
So far this season, weâve had limited persistent weak layers to deal with. Februaryâs periods of calm weather developed a couple of weak layers and problematic interfaces that later got buried in the snowpack. On a whole, weak layers have been short-lived and have generally resolved within a couple of days of being buried. While the following weak layers are no longer major concerns, some readers may want a more in-depth understanding of them before venturing into the mountains.
In the Stevens Pass and East Central zones, the February 4th interface consisted of a thin layer of small (0.5-1.0mm) facets sitting on the stout February 1st melt forms (crust). The crust was widespread on all aspects up to at least 7500ft and the facets were most prominent on the northern half of the compass (west through north through east aspects). A major storm and avalanche cycle February 4th-7th totaled over 60 inches of snow. The February 4th interface was responsible for widespread avalanching including slides up to size D3 at most elevations. As direct action avalanches subsided, the February 4th interface was deeply buried and didnât produce further triggered avalanches. Interestingly, as recent as February 18th, this interface was found in a profile and produced some mixed and head-scratching test results. While this interface is not a concern for triggered avalanches, you may still be able to find it 4-6 feet below the surface, especially on sheltered, shaded slopes at upper elevations.
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A profile from 6460ft on a northeast aspect in the Chiwaukum Range on February 18th shows the February 4th layer. Small column tests produced sudden planar results while a Propagation Saw Test did not indicate propagation.
A more elusive and problematic layer for triggered avalanches was the February 13th interface. This was also most prominent in the Stevens Pass and East Central zones in addition areas of the West Central and Snoqualmie Pass zones. At Stevens Pass a combination of large (2.0-4.0mm) surface hoar and small (0.5mm) near-surface facets developed on a variety of surfaces and were buried on the 13th. The weak layer was most problematic on east through south aspects between 4,500-6,000ft, where the grains were preserved as they rested on a thin crust. It seemed that outside of this aspect and elevation range either 1) the weak grains did not persist enough to be triggered by travelers or 2) the underlying layer, or bed surface, wasnât hard enough for the weak layer to be reactive. A number of parties reported natural and triggered avalanches on southeast aspects during the storm cycle on Presidents Day weekend. This included a party of three that were uninjured after all being caught, with two full-burials, in a surprising avalanche near Skyline Lake on the 17th. As of February 20th, the interface is 1-3 feet below the surface and has become difficult to trigger. The February 13th interface is still visible in the snowpack and we continue to monitor it. It will likely become inactive before the end of the month.
In summary, February has been a great time to explore the mountains and enjoy the longer days for recreating in this seasonâs robust snowpack. Though, not without complexity and variability. Continue to monitor changing conditions and check the daily avalanche forecasts for the most up to date information.Â
Avalanche Problems
Wind Slabs
Wind affected snow could be seen and felt well below treeline Monday. Just because you’re down in the trees doesn’t mean you’re in the clear. Look for signs the wind drifted the snow into firmer and thicker slabs. Textured snow surfaces, firm hollow snow, and drifts behind trees can all indicate winds slabs may be nearby. When you suspect a slope is wind-loaded, steer around convex rollovers, areas below cornices, and steep terrain at upper elevations. If these wind slabs fail on buried facets or surface hoar they could act in surprising ways. You could see wide avalanches, remotely trigger slides, or cause avalanches to fail low on the slope.
You could experience a bit of sunshine on Tuesday as skies clear and temperatures warm. This will cause the snowpack to change. Monitor changes in conditions as you travel. You could see natural loose wet avalanches shedding from steep rocky slopes or cornices failing naturally. Keep in mind what’s above your head, and how it may respond to a warm and sunny afternoon
Release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.
Wind Slabs form in specific areas, and are confined to lee and cross-loaded terrain features. They can be avoided by sticking to sheltered or wind-scoured areas..
Wind Slab avalanche. Winds blew from left to right. The area above the ridge has been scoured, and the snow drifted into a wind slab on the slope below.
Wind slabs can take up to a week to stabilize. They are confined to lee and cross-loaded terrain features and can be avoided by sticking to sheltered or wind scoured areas.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Likely
Expected Size: 1 - 1