Abstract
Three storms intercepted during the Verification of the Origins of Rotation in Tornadoes Experiment generated a moderate-to-strong mesocyclone within the lowest several hundred meters above the ground and qualitatively appeared capable of tornadogenesis, yet did not produce a tornado. Such novel observations of what is considered“tornadogenesis failure” are documented and used to show the insufficiency of a low-level mesocyclone for tornadogenesis. Possible modes of failure are discussed.
Corresponding author address: Dr. R. Jeffrey Trapp, NSSL, 1313 Halley Circle, Norman, OK 73069.
Email: trapp@nssl.noaa.gov