Avalanche Forecast
Regions: Stevens Pass.
Wind slabs may be easy to trigger and act in surprising ways at upper elevations. Loose dry avalanches may be easy to initiate and entrain lots of snow. Travel cautiously and evaluate the bonding of the new snow carefully.
Discussion
Snow and Avalanche Discussion:
The recent snowfall just buried some fairly weak surfaces. The new snow is not bonding well initially, particularly on southerly aspects where the new snow sits over a melt freeze crust, sometimes with facets above. Small dry loose avalanches were observed on southerly aspects of Lichtenberg Mountain on Wednesday. The last slab avalanche we know of in the zone occurred on Sunday, when a climber triggered a small wind slab near the peak of Jim Hill. He went for a short ride, but was otherwise ok.
The weak layer from early February is buried 2-3 feet deep under stout slabs and sits over a crust. It's been over two weeks since observers reported avalanches on this layer. The facets have undergone significant rounding (strengthening) and most snowpack tests indicate that the layer is difficult to trigger. In isolated areas, some snowpack tests are more reactive.Â
A triggered loose dry avalanche (D1.5) through a steep (>40deg) spine-covered rocky slope. 5300ft, NE, Stevens Pass. Photo: Josh Hirshberg
Snowpack Discussion
March 4, 2019
Here we are at the beginning of March. The days are noticeably longer, the sun feels warmer, but the winter is far from over. This may be a good time to take stock of Februaryâs events, where we are now, and what we might expect in the future.
A February to Remember
Many longtime Cascade travelers continue to remark about the long span of high-quality travel conditions in February. Indeed, weâve experienced three weeks of very cold and snowy conditions. Backcountry travelers frequently reported, âbest conditions in yearsâ. February also saw a few rounds of natural and human triggered avalanches. These avalanches were different from our more frequent Cascade storm slabs; here today and gone tomorrow. Most avalanches failed on buried weak persistent layers. As such, most zones spent much of February with Persistent or Deep Persistent Slabs in their forecasts.
Natural avalanche in Icicle Creek Feb 13, 2019. Photo: Matt Primomo
With the notable absence of high elevation rain events, snowpacks around the northwest grew remarkably. On the west slope, most weather stations added 2-4 ft of snow depth. East-side locations added 1-2 ft. Mt Hood locations added 4-5 ft. Even with these impressive snowpack growths, many Cascade Snotel sites are recording near or just below average snow depths for the winter. Â
During most of February, snow conditions were soft and powdery making for fun recreating in many areas. Photo Matt Primomo.
Where We Are Now
Lack of avalanche activity on the layer of buried facets from Feb 8 allows us to gain confidence in many areas. In many areas, there has been a lack of avalanche activity and snowpack tests have been less reactive. These two pieces combined have allowed us to drop persistent slabs from some forecasts and shift others to âunlikely.â The exception is the East Cascades where a shallow snowpack has preserved buried facets, and persistent slabs will remain possible until the sensitivity drops further. So, weâre out to the woods, right? Well, maybe. The same cold and stormy weather that brought us excellent snow quality, also allowed us to bury new weak layers. So far we havenât confirmed any avalanches on these shallow weak layers, but they have our attention and weâre tracking them.
Recently our attention shifted to the upper snowpack. Recent avalanche problems have largely focussed on wind transported snow. Several wind events, predominantly from the east, placed wind slabs on a variety of aspect. With the colder than normal temperatures, wind slabs may not heal as quickly as normal.
A small natural wind slab avalanche in the Crystal Mt backcountry. Photo; Dallas Glass
What Might We Expect
As we move into March, itâs anyoneâs guess what specific weather patterns lay in store of us. However, there are two items that stick out in our minds.
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The strength of the March sun: You can already feel it just walking around town. As the sun creeps higher into the sky and the days grow longer, the sun can have a greater impact on the snow surface. When the sun comes out, expect things to change quickly. You may see avalanches conditions change with natural loose avalanches originating from sunny slopes, surface snow becoming thick and heavy, and slabs taking on a moist to wet snow character.Â
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High elevation travel: Frequently March begins to usher in a period where we push higher and deeper into the mountains. Remember, we donât have as much information about these far-flung locations. If you use the longer days of March to travel to bigger objectives, keep your eyes open. When observations donât line-up with the avalanche advisory, you may be experiencing a different snowpack. Itâs times like these we need to stop and reevaluate.
Mt Baker on a nice day in early February. Photo: Lee Lazzara
February was amazing! but March is here⦠thereâs still plenty of winter left. Stay safe out there.
Avalanche Problems
Wind Slabs
With a shift to southwesterly and stronger winds, the new low density snow will be easily transported on exposed upper elevation slopes and ridgelines. Any fresh drifts may become quite sensitive and turn into wide avalanches as they may form over weak, faceted snow. Be careful to consider these slabs and how even a small slab may be dangerous in consequential terrain. Look for cracking with these drifts. Ridgetop terrain and exposed gullies are the most likely to hold these slabs. Avoid them if they appear to be thick enough and cohesive enough to crack.
Out of the wind effected areas, loose dry avalanches may become common. These may be pack a punch and can run far and fast, particularly on southerly aspects where the new snow is sitting on a thin melt freeze crust. Avoid lingering beneath steep slopes if you see signs of recent loose slides such as fan shaped avalanches and small, fresh debris piles. Remember, most avalanches happen during a snowfall event.
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