Wind Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 1–1.5
It’s time for a mindset shift — snow is back, and so are avalanches. Early in the day, triggering a slide may be difficult with only a few inches of new snow. But as winds increase and snowfall continues, thicker wind slabs will form, and that’s where human-triggered avalanches become more likely. Near the top of the lower elevation band, you might find drifts large enough to trigger a small avalanche by the end of the day - if the old snow surface isn't too bumpy.
It will be easy to track the depth of the soft, new snow over the firm underlying layer. For now, we expect all avalanches to be limited to the new snow. Old surfaces are predominantly hard and bumpy, which could make it harder for new snow to slide over it, especially when the new layer is quite shallow. There could be a few isolated pockets of weaker surface snow, making slides easier in those spots.
During your outing, track new snow amounts and watch for signs of wind loading, like textured surfaces or pillow-shaped drifts. Feel for firmer snow beneath you. Drifts will collect in gullies, along ridgelines, and around features like rocks and steep rollovers. With a shallow new snow layer, simple hand pits in thicker drifts can reveal how easily the snow is sliding. Use small test slopes and watch for red flags like shooting cracks. When in doubt, avoid steep slopes with drifted snow around six inches deep or more — especially as those drifts grow throughout the day.
(1/18/2024)
Example photo: Use small test slopes with drifted snow to see if the new layer slides.
Photo: Julz Holder - Grounding Truth