Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Unlikely
- Größe
- 1
You’ll find recently formed slabs of wind drifted snow on mostly south facing aspects but cross-loaded onto other aspects behind wind breaks such as cliffs and bushes. These slabs are likely to be small unless snowfall totals exceed the forecast. Older and even more stubborn wind slabs can be found on other aspects in the lee of a west wind. These slabs developed late last week and have not resulted in any reported avalanches. Some of these may be on the larger side in the northern part of the range which received much more snow during that upslope snowfall event.
These wind slabs are best described as islands of snow on an icy frozen snow surface, not a complete covering of snow everywhere. In many locations the new snow is very thin or non-existent. What remains is the older refrozen bed surface responsible for multiple skier sliding falls over the weekend with serious injuries as the result.
This avalanche problem may be an attractive surface to climb and ski but remember the unforgiving surface just beneath this new snow. If the lighting is good, the snow surfaces can be easy to identify: new snow will be white, clean while the icy refrozen old surface will be slightly gray in color and reflective at obtuse angles to the sun.