Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1.5–2.5
Moderate WSW Friday night into Saturday morning will continue to move large amounts of low-density snow. Slabs will be reactive in wind-loaded areas, particularly during and just after periods of stronger wind transport. While we're focused on recent slab formation on typical aspects, SE winds earlier in the storm created very large slabs that released naturally on Mt. St. Helens. Similar slab formation conditions on Mt Hood suggest that isolated very large avalanches may lurk, but would be stubborn to trigger. Wind slabs tend to be longer lived than other slab avalanche problems, so don't let your guard down after the winds calm down. As the visibility improves, start to note visual clues such as textured snow, lens-shaped pillows, and fresh, sharp, and very sensitive cornices that point toward reactive slabs on the slopes below. Challenging uphill travel often means that you have a denser slab atop lower-density layers. Propagating cracks and significant settlement serve as reminders to avoid wind-loaded slopes above treeline. Avalanches will increase in size with more widespread potential for large avalanches and isolated very large avalanches above treeline.
(3/10/2023)
Crowns spotted by scientists for the USGS in the neighboring WS zone at Mount St. Helens. These avalanches likely occurred overnight on 3/9 during the height of the storm.
Photo: Wes Thelen