Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
A strong storm system has arrived and will persist throughout the daylight hours. As snowfall rates intensify and strong south and west winds begin to blow, dangerous avalanche conditions will develop near and above treeline on slopes steeper than 35 degrees. Wind slabs will be possible at all elevations, with the strongest presence near and above treeline. Expect wind loading to occur on leeward W-NW-N-NE-E aspects, with SW and SE aspects subject to cross-loading. Drifts will form fast and thick on the leeward sides of ridgelines, cliff bands, and convex rollovers. In the right areas, slab depth will be deep enough to bury you. Observe for growing signs of instabilities, like large shooting cracks, recent avalanches, and active wind loading, as these signs indicate avalanche danger is present. Consider the rate of surface slab growth, and its cohesive properties. Using representative and inconsequential test slopes is a great way to assess the trend of stability and how the new snow is bonding to old bed surface. Areas worth avoiding are wind effected slopes that sit directly below ridgelines, on steep mid-slope breakovers, or nestled among rocky pockets of terrain. Firm surfaces will receive the new storm snow, and bonding capability may not be adequate in areas that have been previously scoured or formed crusts. Slabs and sluffs of storm snow are possible in steep, protected areas of terrain that host more than five inches of fresh, unconsolidated snow. Today is a scenario where the higher you travel in elevation, and the more you expose yourself to the weather and steep terrain, the more you're going to be at risk. Wind-textured surfaces are evidence of wind loading. Wind slabs will display as stiffened snow surfaces with dune, or pillow-like appearances. Conservative travel and decision-making will help decrease your risk and exposure to this problem.
(3/10/2024)
Cracking. A red flag of avalanche danger, which signifies present surface instability.
Photo: Samuel Clairmont