Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1
Recent wind drifts from Monday's storm event are in abundance in the high country. They are mostly located on the leeward sides of ridge crests and terrain features such as sub ridges and rock buttresses or outcroppings on slopes that face N-E-SE, but cross-loading has occurred on NW aspects as well. Today, be on the lookout for fresh drifts to form on these same aspects as well as S as increasing northerly winds continue to blow and drift snow. Wind drifts are recognizable by their smooth, rounded, or rippled appearance, and cracking is a sign of instability.