Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
You can still trigger an avalanche within the recent storm snow on a variety of structural interfaces up to and over two feet deep today. Failure planes may include graupel, early storm low density snow, and on sun and rain crusts. Absent the tell-tale signs of instability (cracking, collapsing), it's worth pulling out the shovel and performing a few snow tests to gather info on the snow that you're keen to ski or ride. Use test slopes (steep but low consequence terrain) to help gather info for representative terrain.
A couple of fine points for today:
- Graupel (pellet snow) can be a significant weak layer as it often runs downhill and pools at the base of cliff bands or on clear transitions from steep to less steep terrain. It's not uncommon to successfully descend a couloir only to trigger the pocket in the aprons or more benign terrain below.
- Sluffing today is possible in the steepest terrain and may be more likely and problematic on the steep southerly aspects today. Weak snow may have developed above yesterday's sun crusts and this may aid and abet any of the sluffing on these slopes.
- Cornices are generally too large to tangle with and remain highly suspect. Remember 5% of our avalanche fatalities involve cornice fall.