Cascades - North East Avalanche Forecast
Jan 11th, 2020 10:00AM
Another winter storm will maintain dangerous avalanche conditions, especially closer to the crest. A healthy amount of respect is warranted for steep slopes at upper elevations due to uncertainties with our quickly deepening snowpack. Plan to give yourself options to avoid steep slopes, as snowfall during the day will increase the danger of slab avalanches.
Saturday provided a bit of a break in the storm pattern and winds drifted snow into slabs in the higher terrain. Another winter storm is forecast to roll through the zone on Sunday. Harts Pass picked up 1.2" of water equivalent and at least 12" of snow since the morning of the 10th. On Wednesday, observers found that a fairly widespread cycle had occurred on January 6/7th, with a few larger slides that buried Hwy 20 under several feet of debris. In the days leading up to January 6th, a string of instability took place, as folks remotely triggered large avalanches on buried weak layers 2 to 4ft down. This same layer is now likely to be at least 5ft deep.
January 9th, 2020 (The regional synopsis is updated every Thursday @ 6 pm)
As we said Happy New Year and rang in 2020, snow was turning to rain at many trailheads and lower elevation Passes, not exactly the fresh start winter recreationalists had in mind. The snowpack was already looking a little thin throughout the region, especially at lower elevations. Low snow in places like Snoqualmie Pass made backcountry travel difficult and hazardous. NWAC’s snow depth climatology report was showing snow depths 25-64% of normal to kick off the start of 2020.
Things can change quickly in the Pacific Northwest and they did as we entered an extended storm cycle between January 2nd to January 8th. Strong winds, fluctuating temperatures, and heavy precipitation offered few breaks in the weather over this period limiting observations and hampering travel. Despite periods of rain at lower elevations, most areas saw several feet of new snow with big jumps in total snow depths as a westerly storm track strongly favored the West Slopes of the Cascades and the Olympics for the highest precipitation totals.
Total Snow Depth (in) 1/2/20
Total Snow Depth (in) 1/8/20
Heather Meadows Mt Baker
Crystal Mt Green Valley
Paradise Mt Rainier
White Pass Upper
Mt Hood Meadows
We may have started with a shallow snowpack, but most locations increased their snowpack by 70% or more over this storm cycle!
During this extended and impressive storm cycle that included backcountry avalanche warnings, natural avalanches were reported in many areas Jan 6th-7th.
The Stevens Pass area was especially active over the period with over 100(!) avalanche observations made on the 6th and 7th. Professionals reported numerous avalanches in places that they hadn't previously observed avalanches and some paths avalanched multiple times in a 24 hour period. Observers reported a few very large (size D2.5-3) avalanches, originating at upper elevations with deeper crowns that likely formed from wind drifting. Topping off an active couple of days, warming temperatures lead to a widespread loose wet avalanche cycle.
The southern Washington Cascades, the Wentachee Mountains and Mt. Hood either saw less precipitation, warmer temperatures leading to more rain than snow, or some combination of the two and ended up with relatively less active avalanche conditions than areas further north.
A large natural avalanche on Rock Mountain near Berne along Hwy 2 east of Stevens Pass that released Jan 6th or 7th. Photo: Josh Hirshberg 1/7/20
Many small storm slabs released in the Crystal backcountry 1/6-1/7. Pinwheels in the photo suggest loose wet avalanche activity occurred when temperatures rose above freezing and snow turned to rain.
Another active and colder weather pattern is on it’s way. Enjoy yourself out there and be sure to check the forecast before heading out. Remember, NWAC is a community-supported avalanche center and when you submit an observation you make the forecast better!
It’s getting deeper! Photo: Jeremy Allyn
As the snow falls and the winds blow, slabs will continue to form. Be observant throughout the course of the day, as these tend to be the most reactive during periods of heavier snowfall rates. Step, or ride off into virgin snow once in a while, and look for shooting cracks as you travel. Near and above treeline wind is likely to stiffen the new snow, creating strong over weak layering.
If you find signs of instability, steer around fresh drifts that may sit below ridgelines and on open slope features steeper than 35 degrees. In any case, be sure to communicate openly and intentionally as a group to help choose which slopes you may and may not want to enter. A healthy amount of respect for steep slopes at upper elevations is warranted due to uncertainties with the quickly deepening snowpack.
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.
Deep Persistent Slabs
Information from upper elevations is limited, increasing our uncertainty regarding a deeply buried persistent weak layer near and above treeline. What we do know is that at least two large, remotely triggered slabs occurred due to a layer of buried surface hoar, and/or weak snow near a crust. This layer can be found about 5ft below the surface at 6,000ft near Washington pass, but is likely quite a bit deeper at higher elevations and in wind deposited areas. It is becoming deep enough that you probably won't observe feedback such as whumphing or shooting cracks as you travel. New snow and wind drifting may increase the load on these layers.
A healthy amount of respect for steep slopes at upper elevations is still warranted. Give yourself plenty of distance from avalanche terrain above 6,000ft. It may be possible to trigger a deep slab from far away or on connected slopes from below. A small slab or cornice failure on the surface may step down to this deeper layer, creating a much more destructive avalanche.
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.
Valid until: Jan 12th, 2020 10:00AM