Persistent Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible
- Dimensione
- 1–2
Strong northwesterly winds last week raked the mountains and mixed into typically more sheltered locations. The incremental wind drifting built hard slabs ranging from just a few inches to several feet thick that is now buried and obscured by recent storm snow. Although you can find these slabs at any elevation, we've seen the most significant wind loading and slab formation occurring nearing treeline, especially in terrain with large fetches favored by northwest winds. These slabs are slower to heal because they formed above exceptionally weak facet layers. They can also be remotely triggered from below or adjacent to steep slopes where the drifted snow spans onto lower slope angles. The problem is localized to leeward terrain features behind tree fences, on the lee sides of ridged terrain features, and in concave catchments such as gullies. Collapses and shooting cracks are clear warning signs of the problem. Give wind-loaded terrain a wider berth than normal as surface clues have been buried by the recent storm snow: there have been several near misses this week with some slides breaking into lower-than-usual slope angles.