Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Human triggered wet slab avalanches remain possible on near and below treeline NW-N-NE aspects due to the wet and weak facet layers buried under the new snow. During the storm rain soaked these persistent weak layers up to at least 8800 ft. These rain soaked layers will remain very weak until the water in them refreezes. Even though air temperatures have dropped below freezing, an insulating blanket of new snow now exists above these wet facet layers, so they may take a few days to refreeze. Once they do refreeze they will gain strength. Until that time wet persistent slabs will remain a problem. These avalanches could involve the entire snowpack. Fortunately as the wet layers refreeze not only will the snowpack stability improve, but the on the snow recreation quality will also improve.