Cascades - West Avalanche Forecast
Jan 11th, 2020 10:06AM
The alpine rating is Storm Slabs., the treeline rating is , and the below treeline rating is Known problems include
A series of powerful winter storms continue to impact the Mountain Loop area maintaining very dangerous avalanche conditions above treeline. Avoid travel on or below slopes 35 degrees and steeper. Expect the most dangerous conditions by Sunday afternoon as additional snow and wind stress the snowpack further.
Observers in the adjacent Mt. Baker and Stevens Pass areas reported very reactive storm slabs on Saturday, with several natural and human triggered avalanches up to size D2 (large). Most avalanches failed about 1ft deep within recent snow, while some failed deeper on the old/new snow interface buried Friday.
Very dangerous avalanche conditions will continue above treeline as more cold, low-density snow (1500-2000ft snow levels) accumulates over the next 24 hours. Expect the bulk of precipitation Sunday. A Puget Sound Convergence Zone may even form in the afternoon near the Mountain Loop Highway bringing locally heavier snowfall. With all the recent snow, be sure to keep tree well and snow immersion suffocation safety in mind (www.deepsnowsafety.org).
Small storm slab near Stevens Pass Mountain Resort. January 10, 2020. Josh Hirshberg photo
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
Avalanches could fail within new snow layers, or deeper on the old/new snow interface buried Friday. Expect thicker and more reactive slabs at upper elevations and in wind drifted areas. All the new snow needs time to stabilize. Avalanches could occur naturally, especially during periods of heavy precipitation and active wind loading. Watch for obvious signs of unstable snow like recent avalanches, shooting cracks, and collapses. Seek out low-angle, supported terrain away from overhead hazard. Anticipate loose dry avalanches as well. These sluffs could entrain quite a bit of snow, or even trigger slab avalanches as they run downslope.
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.
Valid until: Jan 12th, 2020 10:06AM