Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 3
What happened to the buried persistent weak layer of facets (1-3' deep) that formed during the long dry period in January and February? Yesterday, both Greg and I were in Upper Cottonwoods and were still able to find this layer at the mid and upper elevations. While this layer has become noticeably wet during the record heat this past weekend, the structure is still very weak and as it has been unable to fully cool quite yet. In the Ogden area, I would expect a similar structure at the higher elevations.
Over the past few days, this weak layer received a relatively heavy load of snow that is now putting stress on it, and I'm not ready to blindly trust this layer. I think that we are trending in the right direction and this layer is beginning to stabilize with every night of cooler temperatures, but until the temperatures drop consistently and this layer properly refreezes, I will continue to be suspect of the upper elevation slopes facing northwest to north to east.
What to do? Over the next few days, I would continue to evaluate and look for the layer while out traveling. We want to start watching the trend, and seeing if this layer is truly beginning to stabilize. I would continue to perform numerous extended column tests and hand hardness tests to see if this layer is getting harder to push my hand into, and truly refreezing overnight.
Video from my field day in Upper Big Cottonwood Canyon yesterday.