Avalanche Forecast
Regions: Cascades - North West.
Rapidly warming temperatures and sunshine introduces uncertainty into the forecast, but we think loose wet avalanches will be mostly small and manageable by adjusting your aspect and reducing your slope angle. Evidence of large wet avalanches should make you dial back your plans. If you venture into the alpine, identify and avoid large wind loaded slopes and cross-loaded gullies steeper than 35 degrees and steer clear of cornice formations.
Discussion
Cool temperatures on Sunday won the battle against the strong March sunshine, with little loose wet activity observed, but we expect warming to wind the battle on Monday. Â
We received a report of large hard slab avalanche triggered on Saturday, triggered above treeline. These avalanches are older now and more difficult to trigger, but should keep recreationists leery of wind-loaded slopes at upper elevations for another day or so.
Large snowmobile triggered wind slab avalanche near Bearpaw Mountain (NE, 5800ft) HS-AM-R2-D2-U. One rider was caught and carried but injured. 03/14/20. Photo: Chris Macdonald
Large cornices should be gradually softening, making them increasing threats to the slopes below. They have the potential to trigger wind slabs or loose wet avalanches.
Snowpack Discussion
March 12, 2020 (The regional synopsis is updated every Thursday @ 6 pm)
From March 6th to the 12th the Pacific Northwest experienced a few small storms and a few notable days for people and avalanches. Light to moderate snow accumulated slowly over a period of a few days, and avalanche danger increased from Low to Moderate over the weekend of March 8th. The exception was the West North zone, which won the snowfall competition this week. 18-24â of new snow was observed in the Mount Baker area on the 6th, and 10â of new snow on the 11th. Avalanche danger reached Considerable there for storm slab, wind slab, and loose wet avalanche problems.Â
People, complicated avalanche terrain, and lots of avalanches. Bagley Lakes Basin, West North zone. Photo by Nathan Resick, March 8, 2020.
Loose dry slides initiated by skiers in big terrain. No one was caught or carried. East Central zone. March 8, 2020. Matt Primomo photo.
The snow fell with minimal wind, and accumulated slowly over firm suncrusts or wind stiffened surfaces. Thicker cloud cover inhibited the sun in areas where 4â to 12â of snow accumulated over the course of a few days. Cold overnight temperatures allowed the low density snow to weaken. By the 8th, the clouds broke up enough to allow strong radiation to change snow surfaces. When the sun finally did hit the snow, it quickly caused loose avalanches in steep terrain.Â
An active weekend for people and avalanches:Â
Many areas experienced some form of loose avalanche activity from March 6th to 9th. Sunday, March 8th was the day that recorded the most widespread avalanche activity across the region. The size of these avalanches were directly related to the amount of new snow that had recently accumulated in that area, and the size of the terrain.Â
West North zone on March 8, and West South zone on March 8th. Uphill and downhill tracks got covered by debris. Photos by Zack McGill and Dallas Glass.
We as a community can look back at, and learn from these few days. Numerous human triggered slides occurred, some were slabs but the majority were loose. A number of catch and carries were observed, and many more likely went undocumented. Luckily, no injuries or burials were reported. Observers across the region reported lots of instances where previous tracks got hit with debris, either from human triggered or natural avalanches.Â
As the days get longer and folks begin to step into the alpine zone and bigger terrain more frequently, it is important to keep a humble attitude. Continuously evaluate route selection with potential for loose wet and cornice falls in mind. Check the mountain weather and avalanche forecasts for the most up to date info. Enjoy the backcountry, be safe, and let us know what you see out there!
-MP
Solo snowboarder aired into this slope, and went for a ride but was not buried or injured. Slide took out the corner of a skin track. Bagley Lakes Basin, March 8, 2020, Zack McGill photo.
Wind slab triggered by a skier at 7,500ft next to the popular route on Mt St Helens. The skier wasnât caught or carried. Andy Goodwin photo, March 8, 2020.
Avalanche Problems
Loose Wet
This week promises the first major warming event in some time and with that comes uncertainty regarding when and how loose wet avalanche activity will manifest. After a cool start to the day, warming on Monday will start earlier in the day than on Sunday and may reach 6500 ft by the afternoon. We think this will initiate widespread loose wet avalanches in soft or previously soft snow, but with the small expected avalanche size we have kept the danger at moderate. Be especially careful of steep rocky slopes facing west, south or east. Monitor snow surfaces throughout the day, and keep an eye out for roller balls and pinwheels as signs of wet and weak snow surfaces. Move to shaded aspects or lower angle terrain to avoid the problem. If you start seeing evidence of larger loose wet avalanches, we may be further along in an anticipated avalanche cycle than we thought: In this case, dial back your terrain selection to avoid exposure to all slopes receiving direct sunshine steeper than 35 degrees.
Release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. They generally move slowly, but can contain enough mass to cause significant damage to trees, cars or buildings. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
Travel when the snow surface is colder and stronger. Plan your trips to avoid crossing on or under very steep slopes in the afternoon. Move to colder, shadier slopes once the snow surface turns slushly. Avoid steep, sunlit slopes above terrain traps, cliffs areas and long sustained steep pitches.
Several loose wet avalanches, and lots of pinwheels and roller balls.
Loose wet avalanches occur where water is running through the snowpack, and release at or below the trigger point. Avoid terrain traps such as cliffs, gullies, or tree wells. Exit avalanche terrain when you see pinwheels, roller balls, a slushy surface, or during rain-on-snow events.
Aspects: East, South East, South, South West, West.
Elevations: All elevations.
Likelihood: Likely
Expected Size: 1 - 1
Wind Slabs
Strong and variable winds redistributed recent storm snow into wind slabs at upper elevations. These slabs are getting old and should be stubborn or difficult to initiate, but you may still be able to trigger them with a large trigger on a steep convexity. Winds have come from a wide variety of directions since the last snow event March 10-11, so you will find wind-affected snow on a variety of aspects. Expect wind slabs to grow larger and easier to find as you gain elevation or move into more wind prone areas. Some of these slabs may be hard slabs that break widely and behind you, making them especially difficult to escape. Travel cautiously if venture into the alpine, and carefully look and feel for evidence of wind drifted snow. Take time to identify and avoid smooth pillow-like drifts, areas below cornices, or where you find firm over hollow snow. Defer to supported or less consequential slopes if you find signs of instability like shooting cracks.
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: Alpine.
Likelihood: Possible
Expected Size: 1 - 1