Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Very Likely
- Größe
- 2–3
Several flavors of large destructive avalanches are possible today. The travel advice is simple: stay out of the way. Read the Forecast Discussion below for details on specific avalanche problems other than the Persistent Slab and Wind Slab problems described in detail.
What is it? Triggering powerful, 2-5 foot thick avalanches is very likely. Recent snowfall, wind-blown snow, and rain overloaded the buried weak layers (sugary facets or crust + facet combinations) that produced hundreds of avalanches and tragically resulted in an avalanche fatality in recent days. In areas exposed to the wind, slides could release naturally—on their own. Avalanches could be over 1000' wide and may run to the valley floors.
Where is it? Given that we've received snowfall all but one day since February 26th and 1.5-3 feet in a couple of days, the slabs exist on almost all slopes. Wind-loaded slopes are the most dangerous. Many of the slopes that avalanched last weekend have "reloaded" with fresh, dense slabs.
How can you recognize it? Avalanche terrain includes slopes steeper than about 30 degrees and areas below steep slopes. Wind-loaded slopes have stiffer, denser snow that keeps your skis or sled from sinking deep into the snowpack.
How can you manage it? Stay off of and out from beneath slopes steeper than 30 degrees. Persistent weak layers can fail unpredictably and break significantly wider, deeper, and higher on slopes than you might expect, producing much larger avalanches. Smaller wind slab, loose snow, and storm slab avalanches can trigger larger persistent slab avalanches lower on slopes. You could remotely trigger avalanches from gentle terrain far above, below, or to the sides of steep slopes. Avalanches could be triggered by the second, third, or fourth rider on a slope that initially appears to be stable.
(3/10/2023) These very lage persistent slab avalanches failed in lower and middle elevation terrain on N-NE-E aspects above Croy Canyon west of Hailey. Old ski and skin tracks are visible on the bed surface of several of these avalanches.