Deep Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
Data indicates that the recent snow has consolidated and with that consolidation the lingering storm snow weaknesses have gained strength. However, the old surface hoar buried 20 to 40 cm in the snowpack on some slopes represents a persistent weak layer, and the more consolidated snow above now represents a persistent slab in areas where buried surface hoar exists. So far data has shown that this issue exists in some areas (like Andesite Ridge and possibly Red Lake Peak) but not in others. In addition to this lingering persistent slab issue, today's new snow will likely bury the widespread surface hoar that formed yesterday. This surface hoar will also serve as a persistent weak layer for another much more widespread crop of persistent slabs. These new persistent slabs will remain smaller and shallower since only 2 to 6 inches of new snow is forecasted for today, but human triggering of these of these new persistent slabs will be possible in any areas where new snow buried yesterday's surface hoar and may be likely in areas that receive the most new snow.
Triggering an avalanche from a distance, triggering an avalanche from the middle of a slope, and avalanches that propagate farther than normal are all possible with either the old larger persistent slabs or the new smaller persistent slabs. These persistent slabs will exist on any open near and below treeline slope where the old buried surface hoar exists or where newly buried surface hoar exists. It does not take much of an opening for these slabs to exist in, and they may exist in areas typically thought of as safe.