Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 2
With moderate to strong winds over the past 24 hours and plenty of fresh snow, sensitive slabs of wind-drifted snow are likely to be encountered on all upper-elevation slopes and mid-elevation terrain features that allow for drifting snow accumulation. These drifts could be 6-24 inches deep and up to 100 feet wide. Watch out for signs of wind-drifted snow, such as pillow-shaped deposits, and avoid those slopes.
Outside of the wind zone, the new snow will still be reactive. Instabilities could occur at the interface with the old snow surface or within storm snow itself.
Any avalanches, wind-drifted snow, or the new snow may travel fast and far due to weak grains at the new snow, old snow interface. The Valentine's Day storm buried facets, weak stellars, and surface hoar on many slopes. Yesterday, Drew headed to 10,420' to investigate this layer and found weak snow on almost all aspects. While this layering was noticeable on north-facing slopes, there was no observed cracking or collapsing. On east-facing slopes, collapsing was obvious and primarily occurred on facets and small-diameter surface hoar associated with a buried 2cm melt-freeze crust. It's expected that this layering will settle in a few days but could remain active under any stress, whether from wind or snow. Due to this weak interface, remote triggering an avalanche from a distance remains possible.