Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2–3
Observations made yesterday morning revealed unstable wind slabs that were rapidly increasing in size. SW winds strong enough to drift snow into cohesive wind slabs remain ongoing. The vast majority of wind slabs exist in above treeline and near treeline terrain across NW-N-NE-E-SE aspects. Wind slabs exist to a lesser degree in below treeline areas due to the strength of yesterday's winds. Any wind loaded areas where the slab fails deeper in the snowpack as a persistent slab will allow for more destructive avalanches with wider propagation to occur.
Identify and consider avoiding slopes and gullies where wind drifted snow has accumulated, especially below or adjacent to cornice features and wind pillows. Clues such as recent avalanches and snow surface cracking in wind exposed areas indicate the presence of unstable wind slabs.