Avalanche Forecast

In the last 24 hours, Mt. Baker has added nearly 4.5” of water to the snowpack. Initially, 6” of snow fell Thursday evening, but steadily rising temperatures meant that the majority of the precipitation fell as rain, saturating the upper snowpack. Mt. Baker Pro Patrol reported loose wet avalanches running in the upper 6” snow that fell in the last 24 hours.

Tonight will bring more heavy rainfall with 6000-7000 ft snow levels in the evening lowering after midnight as a cold front approaches. The front should pass through the West North zone around 8 or 9 AM with rapidly lowering snow levels behind the front and a rapid transition to snow around this time. Strong winds in the morning should decrease throughout the day with decreasing light snow showers behind the front. Above treeline areas could see 8” or more of snow while near treeline, expect 2-8.”

Several human triggered avalanches were reported in the Mt. Baker Backcountry on Thursday. Avalanches failed within the recent storm snow we received since Monday, primarily in northerly terrain above treeline. Some avalanches had impressive propagation and grew large (D2). Many natural avalanches triggered by cornice fall were reported as well and looked to have run during the wind event on Wednesday. 

Recent natural avalanche (D2) triggered by cornice fall on a NW aspect at 5600ft on Table Mountain. 01/30/20. Photo: Zack McGill, Baker Mountain Guides

Looking Back at January

As we turn the corner from January to February, this is a good time to look back at the last month’s 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.

Snotel weather stations report well above average precipitation amounts for the month of January. Source: www.nrcs.usda.gov

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. 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 state, 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. 

A small skier triggered avalanche (D1) within new snow on a NE aspect at 5600ft on Mt. Herman. 01/28/20 Photo: Zack McGill

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. It’s 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 you’ll find formed from rain events roughly around January 1-3rd, 7th, MLK weekend, 23-25th, and the 31st.

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, there’s a good chance this stormy pattern will continue at least into early February. We’ll 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.