Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 2
With strong winds overnight and 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 150 feet wide. Watch out for signs of wind-drifted snow, such as pillow-shaped deposits, and avoid those slopes. Any avalanches, wind-drifted snow, or new snow may be sensitive today 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. On Friday, Drew headed to 10,420' to investigate this layer and found weak snow on almost all aspects. While this layering was evident on north-facing slopes, there were no observed signs of cracking or collapsing. However, on east-facing slopes, collapsing was apparent, mainly due to facets and small-diameter surface hoar associated with a buried 2cm melt-freeze crust. Drew's findings, as well as all the overwhelming avalanche activity yesterday, let us know that the southeasterly and easterly facing terrain is the current bulls-eye terrain for this issue. Due to this weak interface, remote triggering an avalanche from a distance remains possible.
It's expected that this layering will settle in a few days but could remain active under any stress, whether from wind or snow today. If this layer does not settle out, we would expect to see it transitioning away from an interface issue and into a more traditional persistent weak layer instability.