Avalanche Forecast
Regions: Mt Hood.
Precipitation, light winds, and very cold temperatures gave Mt Hood a nice blanket of fluffy unconsolidated snow. Don’t let the cold smoke distract you. Be leery of steep slopes where you may trigger loose avalanches that run far and fast on the firm surface underneath.
Discussion
This unique storm has been a tricky forecast for Mt Hood. Despite the close proximity of heavier precipitation, and expected strong easterly winds, Hood remained pretty quiet, with modest new snow amounts and generally light winds. We expect more of the same Sunday.Â
As of Saturday afternoon observations from the area reported 8-10â of very low-density snow with nearly no wind affect. This storm snow accumulated over a wide variety of surfaces including blue ice, wind packed snow, old settled powder, and weak sugary facets. Now that these old surfaces are buried itâs hard to anticipate what lies beneath. If the new snow rest over blue ice, it could make for difficult, if not dangerous, travel conditions.
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 Dry
Chilly temperatures, light winds, and minimal additional snow should allow the surface to remain light, dry, and unconsolidated. As a result, you could trigger loose dry avalanches on slopes steeper than 35 degrees. Some of these slides could run far and fast. Don’t get surprised by these sluffs, knocked off your feet, and pushed into a terrain trap.
Even though we’re expecting mostly cloudy skies, you could see a few sun breaks or periods of filtered sunshine. If you start to notice the sun, odds are, so does the snowpack. This could cause the snow to change and behave differently. You may see the new snow settle into a slab or, if the sun stays out long enough, produce natural loose wet avalanches. If you find the surface snow becoming firmer, see new rollerballs, or find other signs of unstable snow, dial back your terrain use and steer around steeper convex rollovers and higher consequence terrain.
Release of dry unconsolidated snow. These avalanches typically occur within layers of soft snow near the surface of the snowpack. Loose Dry avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs. Loose Dry avalanches can trigger slab avalanches that break into deeper snow layers.
Loose Dry avalanches are usually relatively harmless to people. They can be hazardous if you are caught and carried into or over a terrain trap (e.g. gully, rocks, dense timber, cliff, crevasse) or down a long slope. Avoid traveling in or above terrain traps when Loose Dry avalanches are likely.
Loose Dry avalanche with the characteristic point initiation and fan shape.
Loose dry avalanches exist throughout the terrain, release at or below the trigger point, and can run in densely-treed areas. Avoid very steep slopes and terrain traps such as cliffs, gullies, or tree wells.
Aspects: All aspects.
Elevations: All elevations.
Likelihood: Possible
Expected Size: 1 - 1