Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 4
Andy and I stomped around the North Slope yesterday and the viddy aboveillustrates our problem child, a persistent weak layer (PWL) now buried and perserved underneath about 2 feet of snow. Of course, the stronger snow on weaker snow combo creates the structure resulting in an increase in avalanche activity, and I think yesterday's robust warm up aided in the process as well. In either case, we know we have a deceptively tricky weak layer, it hasn't gone away, and we're seeing the biggest sign of unstable snow... avalanches! But, it's not like there are slides everywhere and place is coming unglued. However, in addition to recent avalanche activity there are also plenty of other red flags like collapsing and shooting cracks. So the safest approach is to assume the PWL is present on shady slopes and remains guilty until proven otherwise.
Where does this weak layer exists? The bullseye locations are basically all slopes with dry powder near and slightly below treeline today. Above treeline, the PWL is not as uniform and a little more pockety in distribution. The scary part about this situation is that this layer and it's ability to produce avalanches is variable.
How to avoid it? There are two options. (1) Ride south facing slopes where this layer doesn't exist but the riding conditions are variable. Or, (2) ride northerly facing slopes with dry powder but avoid being on or under any slope steeper than 30 degrees.