Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible - Likely
- Größe
- 1–2
Reports suggest the recent 10-30 cm is poorly bonded to the interface below (a layer of surface hoar). Keep an eye on the wind, slabs may quickly form wherever the wind encourages the fresh snow to bond; and with a weak layer of surface hoar below, reactive slabs may be more widespread and extend into treeline elevations and be more reactive than expected in sheltered areas.
The "upper" early winter snowpack consists of around 60 cm of recent snow over various layers formed mid-November, including surface hoar, faceted grains, and a hard crust. While our avalanche concern is focused on the interface just below the recent snow, we're hoping to gain more information on the distribution and sensitivity of these deeper layers as we collect more field observations.
Avalanche hazard is unlikely at lower elevations where snowpack depths have yet to overcome ground roughness like brush and rocks.