Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–1.5
Recent field observations suggest Wind Slabs that formed during our brief storm on the evening of 1/3 are most likely to be relatively thin and small in size. However, unstable areas of wind-stiffened snow may still be reactive to the weight of a rider. Keep an eye out for clues that indicate nearby wind deposits, such as recent cornice growth, hollow upside-down feeling snow, and uneven snow surfaces. Be suspect of terrain features that encourage drifting, such as the leeward sides of ridgelines, alpine couloirs, and cross-loaded depressions, and watch for signs of instability, such as shooting cracks in upside-down snow and recent avalanche activity. Be particularly cautious in areas with higher snow totals from our recent storm. This may include higher elevations and areas closer to the crest, as well as the northern reaches of the forecast area.
(12/29/2024)
small 4F wind deposit kicked off on a test slope (~ 10 cm deep) N, NTL, 9900'
Photo: Samantha Rubin