Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Winds have moderated this morning, decreasing to velocities ideal for wind slab formation, and more snow is now available for transport. Yesterday's strong winds blew more snow off the mountain, rather than redeposit as reactive wind slabs. However, our observations were limited, and high elevations may harbor lingering reactive wind slabs in steep/extreme terrain.
KPAC advises backcountry travelers to anticipate new reactive wind/storm slabs and exercise caution, especially above and near treeline. You will decrease your avalanche danger dramatically by avoiding loaded avalanche starting zones, wind drifts, pillowed snow, and cornices. A valuable strategy for evaluating wind/storm slab hazards is to test small, inconsequential slopes, which can provide valuable insights into the reactivity of wind-packed snow on particular aspects and terrain features.
Cornices starting to form at the top of Snowslide Canyon Bowl. (3/30/2024) Photo: Max Campbell