Avalanche Forecast
Regions: Cascades - North West.
Easterly winds will transport snow and create fresh wind slabs near and above treeline. Use caution as you gain elevation and transition into wind-affected terrain. In isolated areas, wind slabs may form on weak old snow surfaces.
Discussion
Snow and Avalanche Discussion
No new avalanches have been reported since the weekend except for minor loose dry sluffs in steep terrain. Over the past two days, the West-North zone experienced sunshine, moderate easterly winds, and blowing snow in upper elevation terrain. On Tuesday night and Wednesday, wind speeds will increase and continue to blow out of the east. Plenty of light snow is available for transport and fresh slabs will form as the winds pick up.
Over the past several days, weak snow surfaces formed during cold, clear periods and were preserved by rounds of low-density snowfall. In some areas, you can find layers of buried surface hoar or crusts/facets in the top 1-2ft of the snowpack. These layers have an isolated distribution and do not exist everywhere. Where they can be found, a slab may or may not yet have formed on top. Track these layers closely - they could become problematic as we get more wind, snow, and building slabs in the coming days.
Snowpack Discussion
February 24th, 2019
The Status Quo
As we look at the avalanche conditions the phrase âStatus Quoâ keeps coming to mind. We use this term in the avalanche industry to note periods of no substantial changes, where observations continue to support the current avalanche danger, and our terrain use doesnât appreciably change. Weâll look at recent avalanche conditions with this lens.
Avalanches
Following several large winter storms just prior to Valentine's Day, we saw very active avalanche conditions. With a few notable exceptions, most of the avalanche activity occurred more than a week ago. This lack of activity has allowed us to gain some confidence with the persistent weak layer buried on February 8th. You can see this reflected in the progression in the likelihood of persistent slab avalanches from âLikely,â to âPossible,â to âUnlikely.â The timing of this progression has been different depending on the zone.
The recent exceptions were two very large avalanches in the Crystal Mountain area on February 20th. During avalanche mitigation work, Crystal Mountain Ski Patrol triggered a slide on a SE aspect at 6300 ft in a less often skied portion of their ski area. On the same day, a skier triggered a persistent slab on a W aspect at 6300 ft in the backcountry adjacent to the ski area. Both were 3-4 ft deep. Itâs hard to ignore these two obvious signs of instability.
Feb 20, 2019: SE 6300â: SS-AE-D3-R3-O. Photo: Crystal Mt Ski Patrol
Snowpack
Snow profiles and snowpack tests have been coming in from nearly every region. This is great! It helps us put together a more complete picture of the snowpack structure. Observers continue to report a layer of facets 2-5 feet below the snow surface and just above a crust. These facets are showing signs of rounding (gaining strength). In the past week, snowpack tests have become more variable. Some tests are indicating triggering an avalanche and crack propagation (necessary for a slab avalanche) are becoming less likely. That said, we are still seeing other tests that indicate that triggering deep persistent slabs remains a possibility. More tracking of this trend is needed to concretely illustrate the trend.
The Feb 8 facet layer is 3-5ft deep in the Snoqualmie Pass area. Â Photo: Susie Glass
Weather
Our recent weather systems have not been big water producers, especially by Cascade standards. However, the colder than normal temperatures have produced light, low-density snowfall. Wind transported snow have been the main driver of slab avalanches in the new snow. These storms have been large enough to keep the avalanche danger elevated, but not enough for major spikes in danger.
Recent low-density snow drifted by the wind to form fresh slabs Photo: Dallas Glass
Looking Ahead
At this point avalanches on persistent weak layers canât be fully ruled out on specific aspects or elevations in most zones. Your chances of triggering an avalanche on a persistent weak layer are lower than they were on February 13th, but the change from day-to-day will remain slow and incremental. As a result, youâve seen slow changes in the avalanche danger in most zones. Due to the serious consequences and the uncertainty that these avalanches present, we will continue to operate with a âStatus Quoâ mindset. Donât let this lack of change lull you to sleep.
When will the conditions change? Not tomorrow, but possibly within the next week or two. Keep checking the forecast. Make sure to read the Snow and Avalanche Discussion and the Avalanche Problem text so you can stay up to date with any changes as they arise.
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Avalanche Problems
Wind Slabs
Easterly winds will continue to drift snow and create fresh slabs. Older wind slabs that formed over the weekend still exist. In isolated areas, you may find wind slabs resting on buried surface hoar or on crust/facet layers. You are most likely to trigger a wind slab in complex terrain at upper elevations. Watch for blowing snow, drifts, textured surfaces, and stiffer slabs on leeward sides of ridges and in wind exposed terrain. Steer around wind loaded slopes near and above treeline steeper than 35 degrees.
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: Alpine, Treeline.
Likelihood: Possible
Expected Size: 1 - 1