Avalanche Forecast
Regions: Mt Hood.
Very little is changing as a new period of strong east winds combine with cold low-density snow to refresh wind slabs on lee slopes, mainly below ridges. Shallow wind slabs are possible even on open slopes below treeline. Large deep slab avalanches remain possible in this zone. Choose well-supported terrain and avoid large open slopes where avalanches can start.
Discussion
Snow and Avalanche Discussion
A pattern of strong winds and new snow has been repeating itself nearly daily for several days, keeping wind slabs front and center. Winds freshened Tuesday, strong enough to continue transporting snow and building new fresh wind slabs.
A previous round of fresh snow and strong NE winds Monday formed wind slabs on non-typical aspects. No backcountry observations were received Monday. Avalanche control results do not tell the true story for backcountry terrain where avalanches would be much larger and more dangerous than those seen in the ski areas the past few days.
Prior to Sunday's new snow, professionals digging in the snow and looking for the 2/8 weak snow/crust combination in the Mt. Hood Meadows area were finding it roughly 4 feet down on N-E aspects and in a rather narrow elevation band around 5300’-6000'. Â
While this is very useful and specific information, we can't extrapolate this to the larger Mt. Hood area to fine-tune the suspect aspects.
Temperatures have been very cold and combined with strong winds, be prepared for very harsh winter conditions and the threat of frostbite or hypothermia.
With all the low-density snow piling up the risk of a Tree well/Snow immersion and Suffocation accident continues. Unfortunately, there was a tragic tree well/SIS fatality at the Timberline ski area on Saturday.
Snowpack Discussion
February 24th, 2019
The Status Quo
As we look at the avalanche conditions the phrase “Status Quo†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 doesn’t appreciably change. We’ll 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 “Likely,†to “Possible,†to “Unlikely.†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. It’s hard to ignore these two obvious signs of instability.
Feb 20, 2019: SE 6300’: 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 can’t 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, you’ve 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 “Status Quo†mindset. Don’t 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
Strong east winds developed Tuesday and should continue Wednesday and will continue to easily transport low-density snow and form fresh and sensitive wind slabs on lee slopes, especially below ridges. Winds may be strong enough to form wind slabs on open slopes below treeline, so keep your eyes opened for wind stiffened snow even below treeline.
Steer around slopes steeper than 35 degrees where wind slabs have likely formed, using visual clues like textured snow, blowing snow and fresh drifts. Feel for firm or hollow snow. If you can't tell which slopes have been loaded, choose lower angled terrain.
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: Likely
Expected Size: 1 - 1
Deep Persistent Slabs
The 2/8 persistent weak layer/crust combination we have been tracking is only getting deeper with each passing storm and there haven’t been any reported avalanches on this layer in over a week. However, the snowpack structure remains the same and with deep persistent slabs, long stretches of time may pass between triggered avalanches.
You are unlikely to experience warning signs like cracking or whumphing given its depth. It may take finding a shallower spot in the snowpack where you can trigger an avalanche on this layer or a smaller avalanche that steps down to this interface.
Let this low-likelihood/high consequence avalanche problem determine your terrain choices, avoiding terrain capable of producing large avalanches.
Release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer, deep in the snowpack or near the ground. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage. They commonly develop when Persistent Slabs become more deeply buried over time.
Deep Persistent Slabs avalanches can be destructive and deadly events that can take months to stabilize. You can trigger them from well down in the avalanche path, and after dozens of tracks have crossed the slope.
A snowboarder triggered this Deep Persistent Slab near treeline, well down in the path.
Deep, persistent slabs are destructive and deadly events that can take months to stabilize. You can triggered them from well down in the avalanche path, and after dozens of tracks have crossed the slope. Give yourself a wide safety buffer to handle the uncertainty, potentially for the remainder of the season.
Elevations: Treeline, Below Treeline.
Likelihood: Unlikely
Expected Size: 1 - 2