Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 2
Yesterday, the snowpack was chatty as new snow and wind overloaded our persistent weak layer -- Red flags were everywhere!
The storm snow and wind we received this weekend formed a dense slab that we were missing from our snowpack structure. Above 9,000' on the north half of the compass, old snow grew weak and sugary over the past month and is now buried between 1-3' beneath the slab. Because of this, avalanches are now breaking 1-2' deep and up to a couple of hundred feet wide on the persistent weak layer near the ground. It is a great time to break out the shovel and take a deeper look under the snowpack's hood. Some quick excavation will reveal a dense slab over weak sugary snow. This is what creates the trap-door feeling when trenching our sled or ski track.
I am most suspect of upper elevation terrain on steep and rocky slopes where there was enough snow to ride prior to this storm. Remember, the tricky thing with persistent slab avalanches is that we are able to trigger them remotely, or from a distance away.
Above, you can see and Extended Column Test yield results that suggest increased sensitivity in the snowpack breaking on persistent weak layers in the lower portion of the snowpack.