Avalanche Forecast
Regions: Cascades - North East.
Dangerous avalanche conditions are developing with steady snowfall, strong winds, and rising temperatures. If you choose to go out on Wednesday, be mindful of all steep slopes. This storm will not let up until Friday.
Discussion
Another atmospheric river is knocking at our doorstep, and may be here by the time you read this. Expect Wednesday to be a dynamic day with increasing danger. Avalanche conditions will become dangerous as more snow falls, temperatures warm, and winds crank up to full speed. This may happen more quickly in upper elevation terrain, but by later in the day, warming temperatures may increase danger at lower elevations. The recent cold temperatures have created weak, sugary (faceted) snow surfaces, and new snow may not bond well. Wednesday is not a day to hang it out there as this storm is expected to create High danger by Thursday.
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Snowpack Discussion
January 30th, 2020Â (The regional synopsis is updated every Thursday @ 6 pm)
Looking Back at January
As we turn the corner from January to February, this is a good time to look back at the last monthâs snow, weather, and avalanche conditions. January was notable for continuous storms and elevated, yet quickly resolving avalanche danger. In most parts of the region, the snowpack grew significantly. Snow depths went from far below average at the New Year to near normal by the end of the month. While numbers are still being compiled, January 2020 could rank high for total precipitation amounts in some locations. As we move forward, there are currently few layers of concern in the existing snowpack.Â
Snotel weather stations report well above average precipitation amounts for the month of January. Source: www.nrcs.usda.gov
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Weather
January was marked by an onslaught of storms with very few breaks in precipitation lasting 24, or even 12 hours. Most notable was the sheer amount of precipitation that these storms delivered. Most NRCS Snotel weather stations are reporting at least 125% of average precipitation amounts for January, with many over 200% of average. Not all of this fell as snow. For the month of January, the Mt. Baker, Snoqualmie Pass, Paradise, and Mt. Hood Meadows weather stations measured an astounding 42â, 33â, 32â and 28â of water (both rain and snow) with 1 day still left in the month. If you do some quick math, those 4 stations average near or above an inch of water a day! Â
Snow levels and temperatures were less consistent than the overall stormy weather. On the heels of a warm December, the first week of the New Year followed suit. From about January 8th through the 19th a cold period had its grasp on the region, bringing snow to the lowlands and copious amounts of light, champagne powder to the mountains. The last third of the month saw continued storms. Temperatures moderated and warm air brought occasional rain to middle and even upper elevations.Â
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A small skier triggered avalanche (D1) within new snow on a NE aspect at 5600ft on Mt. Herman. 01/28/20 Photo: Zack McGill
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Snow and Avalanche Danger
After a meager start to the winter, the snowpack grew exponentially in January. In fact, the storms were so intense in the middle of the month that they challenged the accuracy of remote weather stations. Snow blocked precipitation gages and knocked out cellular towers and phone lines used to transmit data. Currently, snow depths from reporting sites are near average.
While the storms often brought rapid spikes in avalanche danger, the hazard was quick to taper off. Throughout the month, there were 12 days when NWAC issued High Danger in one or more zones and 11 days when there was at least some Low Danger in forecasts. Itâs notable that there were no days with all Low Danger in any forecast zone. In addition to the snowpack growth, a positive side to the storms was that weak layers had little time to form. In general, any facets or surface hoar that formed were very short-lived weak layers. Most avalanche problems involved new snow, wind or wet snow. There are still some areas of shallow, weak snowpack in typical places like the Wenatchee Mountains and the most eastern extent of the Cascade Mountains. Aside from that, the snowpack layering in most zones is marked by a few lingering storm interfaces in the upper snowpack and intermittent crusts from rain events. If you dig in the snowpack around the region, the most prominent crusts youâll find formed from rain events roughly around January 1-3rd, 7th, MLK weekend, 23-25th, and the 31st.
Looking Forward
The winter snowpack is now well established for recreating and traveling through the mountains. Much more so than it was a month ago. Looking ahead, thereâs a good chance this stormy pattern will continue at least into early February. Weâll keep monitoring how the snowpack continues to change near the surface with each weather event. You can check the daily Avalanche and Mountain Weather forecasts for the most up to date information.Â
Avalanche Problems
Wind Slabs
Strong winds are quickly drifting the new snow into cohesive slabs. These slabs may occur naturally and may be easy to trigger as they are resting on weak snow surfaces. Stay off of steep slopes where you find cohesive slab buildup and observe shooting cracks nearby. The most likely places for natural slab avalanches will be just below high ridgelines where the new snow loads and on open slopes with drifting across them. Be aware of what is above you, as you may be able to trigger slopes from below. If you choose to go out on Wednesday, be very mindful of all steep slopes.
Rain on snow by mid day will cause a cycle of loose wet avalanches at lower elevations. Look for signs such as roller balls, and gloppy snow with dry snow underneath to clue you in. Avoid steep slopes as soon as you find these signs. Loose wet avalanches may run far at lower elevations on Wednesday.
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: All elevations.
Likelihood: Likely
Expected Size: 1 - 1
Storm Slabs
Warm, heavy snow resting over cold, lower density snow may create reactive storm slab conditions. Look for these to begin occurring where you find about 8" of new snow, and if you observe heavy snowfall rates. These may happen outside of wind affected areas. Avoid convex and unsupported slopes, and terrain traps like gully bottoms and avalanche path runout zones.
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.
Elevations: Treeline, Below Treeline.
Likelihood: Likely
Expected Size: 1 - 1