Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–2
Below treeline (& possibly up to 2300m): High freezing levels and rain events created a rain crust (or two). New snow is not bonding well to these near surface rain crusts. Rain crusts are more prominent in the southern / central Purcells.
At and near tree line, the new snow rests on widespread layer of large surface hoar crystals. Shooting cracks, remote triggering and settlements (whumphing) are classic signs of instability that buried surface hoar is present and potentially reactive. Snow that has been wind affected may be most reactive. We suspect this Surface Hoar is most intact in areas that saw little rain (& hence have no THICK rain crust).
At upper elevations where recent winds transported new snow, storm slabs formed in lee features (Northerly and Easterly slopes) and will be especially touchy where they sit over a crust.