Avalanche Forecast

Issued: Feb 16th, 2020 10:00AM

The alpine rating is considerable, the treeline rating is moderate, and the below treeline rating is moderate. Known problems include Wind Slabs.

Northwest Avalanche Center NWAC, Northwest Avalanche Center

Email

Pay particular attention Monday if you travel in areas where the wind drifted the snow, to higher elevation locations, and/or on the volcanoes. Steer around convex rollovers, steep wind affected slopes, and terrain greater than 35 degrees at upper elevations.

Summary

Discussion

The West-South zone seems to once again be demonstrating its diversity. Areas close to Mt Rainier, Mt Adams, and Mt St Helens should continue to see the greatest snow accumulations Sunday night and Monday morning. With limited observations, we have lower confidence in conditions in these same areas. If you travel on or near one of the volcanoes, ease into the terrain by starting with smaller and lower consequence slopes to gather observations and test the forecast. When in doubt seek out lower angle terrain.Observations from the West South on Sunday indicated the most reactive snow lay in wind loaded areas and where the greatest snowfall accumulated over a recent crust. A party traveling in the Crystal backcountry remotely triggered a wind slab from near ridge crest. The avalanche was 18-30” deep, 60’ wide, and ran on the prominent 2/13 crust. 

Remotely triggered slab avalanche in the Crystal backcountry. Cement Basin, E Aspect, 6500’. SS-ASr-D2-R1-I Photo: Jeremy Allyn.

Snowpack Discussion

February 13, 2020 (The regional synopsis is updated every Thursday @ 6 pm)

Heart of Winter

The action has been non-stop so far in 2020 with several widespread natural avalanche cycles and a few recent close calls. The active weather pattern has kept us all on our toes, especially January’s barrage of storms bringing seemingly endless precipitation and dramatic snowpack growth. Ongoing snow, wind, and rain continued into February, and a not-so-ordinary atmospheric river event recently left its mark on the region. The second week of February brought the first stretch of high pressure in weeks, allowing the snowpack to gain strength and the avalanche danger to ease between storms. Now, in the heart of winter, we have a deep and healthy snowpack with snow depths throughout the Cascades and Olympics near 100% of normal. Looking ahead, each day brings new changes to the upper snowpack, and a dynamic pattern with direct action events (storm-driven avalanche danger) will likely be par for the course.

Atmospheric River Aftermath 

Model simulation for February 5-6th, 2020 showing an Atmospheric River (AR) with a less than common northwest-southeast orientation as it impacts the region. This orientation allowed for strong westerly winds and more favorable upslope flow than a more typical AR approaching from the southwest. Image courtesy of the Center for Western Weather and Water Extremes, UC San Diego. (Link)

An atmospheric river impacted the region on February 5th-8th, causing a string of notable events. This storm favored the Central Cascades and Stevens Pass in particular, which experienced continuous heavy snow and rain for 86 hours, amounting to almost 70in of snow with about 7.5in of water equivalent. Not surprisingly, atmospheric rivers often go hand in hand with avalanche warnings, which were issued for 3 consecutive days at Stevens Pass from February 5th-7th, along with high danger in all other zones. Heavy rain fell at low elevations and even caused a significant mudslide on SR 410 between Enumclaw and Crystal Mountain, closing the road for 4 days and knocking out communications to 9 mountain weather stations for a week. As the AR exited the Northwest, and natural avalanche activity tapered off, conditions still remained touchy to human traffic on February 8th and 9th. Several triggered avalanches were reported that weekend, most notable of which was a close call near Mt. Baker Ski Area:

On February 8th, a skier was fully buried in an avalanche adjacent to Mt. Baker Ski Area. The avalanche was triggered by a traveler from a different party. Mt. Baker Ski Patrol was on the scene immediately, located the victim quickly, dug them out, and cleared the airway. The individual survived and reported no injuries. The avalanche was about 1ft deep and eventually broke up to 500ft wide. NNW aspect 5500ft. Photo: Mt. Baker Ski Patrol

Clear skies on Sunday, February 9th gave observers a chance to document the widespread avalanche cycle in the Stevens Pass zone that occurred February 5th-8th, including this view of crowns from large natural avalanches in the Berne Camp Chutes with Glacier Peak in the background. Photo: Matt Primomo

High Pressure before President’s Day Weekend

The week of February 10th brought the longest stretch of dry weather so far in 2020. A notable northwest wind event redistributed snow throughout the region and drove an isolated wind slab problem in most zones. Generally, it was the quietest few days avalanche-wise in weeks. However, a significant human-triggered avalanche occurred near White Pass on February 12th. Fortunately, no one was caught or injured. The incident provided a good reminder that even during periods of lower avalanche danger when avalanches are unlikely, outlier events can and do happen. The winter snowpack will always pose some level of uncertainty, and big triggers like cornice fall can produce surprising results.   

The crown of a human-triggered avalanche on a northeast aspect at 6700ft in the Hogsback area near White Pass. Two travelers unintentionally triggered a cornice, which dropped onto the slope below and triggered a very large avalanche. 2/12/20 Photo: White Pass Ski Patrol

Problems

Wind Slabs

An icon showing Wind Slabs

Another round of wind and snow Sunday night will continue to build and grow wind slabs. Keep your eyes peeled for clues the wind drifted the snow into slightly thicker and firmer slabs. Fresh cornices, drifts behind trees, and textured snow surfaces all indicate the wind affected the snow. With such strong winds, you could find wind loading on exposed slopes at any elevation and along the sides of mid-slope gullies. When you suspect the wind drifted the snow, steer around convex slopes, areas below cornices, and steep slopes at upper elevations. Avalanches should be the largest near ridgecrest and above treeline.

Cornices during this period grew large and overhanging. Many travelers reported sensitive cornices along ridgelines this weekend. Give these sleeping giants a wide berth. If the sun comes out you could see cornices fail naturally and impact the slopes below as a very large trigger. This same sunshine could also drive a natural loose avalanche cycle from very steep and rocky slopes. Don’t let these natural cornice collapses and loose wet avalanches catch you lingering on slopes below. 

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

Valid until: Feb 17th, 2020 10:00AM