Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1.5–2.5
Areas of unstable snow are expected to form first on slopes that are filling in with wind loaded snow, spreading to include wind protected areas below treeline as the day progresses. Identify areas where visible drifting snow is depositing and filling in on slopes of concern. Signs of unstable snow include cracking, collapsing, or recent avalanches. These clues to unstable snow are expected to spread to wind protected slopes below treeline as the day progresses. Identify slopes that hold potentially unstable snow and consider avoiding them. Tighten up your travel practices today. Focus on very clear communication within your group and do not rely on marginal islands of safety in or below avalanche terrain.
High intensity snowfall will rapidly create new storm slabs today. Once new snow amounts surpass 6+ inches, all avalanche terrain will become suspect. Where the additional new snow load is added above the weak, faceted (sugary) Feb 10 layer across NW-N-NE aspects, avalanches could break wider than expected or trigger from lower on the slope than expected. Any collapses or whumpfing noises indicate that you have found a slab on top of the Feb 10 layer. The same advice applies here: Identify slopes that qualify as avalanche terrain and consider avoiding them.
Snow surface cracking like this indicates that you have found unstable snow. Where this is the case, consider opting for slopes with a slope angle under 30 degrees until you have navigated away from avalanche terrain.
This photo was taken earlier this year near Blue Lakes, CA.
Photo: Jason Bilek