Wall cloud
Wall clouds (or pedestal clouds) are localized, large and persistent lowering cloud formations that develop below the rain-free region of thunderstorms. Rotating wall clouds are indicative of mesocyclones in thunderstorms. Wall clouds do not always rotate, though.[1]
Wall clouds are formed by a process known as entrainment, when an inflow of warm, moist air rises and overpowers rain-cooled air during a downwind downdraft.
Wall Cloud Media
Position of Wall cloud under a supercell storm.
A wall cloud with tail cloud.
A shelf cloud over Enschede, Netherlands
Classic supercell thunderstorm
A tornadic wall cloud with RFD clear slot.
References
- ↑ Higgins Storm Chasing | What are Wall Clouds? (in en-US). Retrieved 2022-03-27.
