Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2
Winds have been drifting snow at all elevations into thicker slabs. Though they are still fairly soft in most areas, they could be larger and more dense in alpine terrain. Slabs may rest over weaker surfaces and could react in surprising ways. NW-NE aspects are likely to hold weaker, faceted snow and are the most suspect. These aspects have consistently produced collapsing and shooting cracks in the low 4,000ft range (quite low in elevation). There is uncertainty with higher elevation, alpine terrain but expect that large and wide avalanches could be triggered. One slope may avalanche, while another may not due to the variable nature of old snow surfaces.
Travel conservatively knowing that you could trigger a surprising avalanche in some areas. Monitor how the new snow is bonding to older layers, and check for weak faceted grains over a stout crust beneath the storm snow. Look and feel for wind stiffened snow as you gain elevation, and look for shooting cracks or whumphing collapses - these are signs of instability that should be heeded.
(1/31/2022)
Large, remotely triggered wind slab avalanche on Shuksan Arm in West North zone. NW aspect @ ~5400'. Rain-affected crust/old snow surface is visible as the bed surface.
Photo: Liza Kimberly