Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–1.5
Signs of wind slab instabilities are beginning to wain in the West South. As this happens, the problem may migrate into steeper and more complex terrain. The odds of triggering an avalanche will increase with slope angle, where the slab is thicker, and the slope is less supported. Convexities, tops of chutes, aprons at the base of cliffs, and slopes below steep ridgelines are all likely locations to find this problem. You will probably see lots of signs of wind transport, but determining which slope is reactive will be trickier. You can use hand pits and small test slopes to gauge for reactivity, but you need to be sure that the test slope is representative of the start zone on the slope you are considering. Subtle differences in slope angle, aspect, and wind-deposition patterns can make a huge difference in slab presence and reactivity. Carefully assess the slope in question and if you decide to travel on it, only expose one person at a time and keep eyes on your partner. Choose well-supported and planar slopes without signs of wind-loading to put the odds in your favor.
(12/15/2024)
A heavily wind-loaded northerly slope. You can tell how "fat" it is by the textured surfaces and pillow-like drifts. Be cautious of steep and wind-loaded slopes below steep ridge lines like this one.
Photo: Andy Harrington