Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1
Wind slabs linger on shaded aspects while a fresh round of winds from the ESE may form some shallow slabs onto atypical aspects. Note when you move into colder drier surface snow and whether the winds are transporting snow near ridgelines. If they are, slabs may be forming on more W-facing atypical aspects. Some older slabs may remain reactive near ridgelines, so check representative test slopes for cracking and propagation before engaging with more committing slopes at upper elevations.
Example: Signs of wind-transport on a ridgeline. The scalloped features (sastrugi) point to where the wind came from. The cornice is also a red flag. Below sharp ridges like this are where lingering wind slabs may be found to start to day.
Photo: Andy Harrington