Abstract
Over the last decade, supercell simulations and observations with ever-increasing resolution have provided new insights into the vortex-scale processes of tornado formation. This article incorporates these and other recent findings into the existing three-step model by adding an additional fourth stage. The goal is to provide an updated and clear picture of the physical processes occurring during tornadogenesis. Specifically, we emphasize the importance of the low-level wind shear and mesocyclone for tornado potential, the organization and interaction of relatively small-scale pretornadic vertical vorticity maxima, and the transition to a tornado-characteristic flow. Based on these insights, guiding research questions are formulated for the decade ahead.
Original language | English (US) |
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Pages (from-to) | E1084-E1097 |
Journal | Bulletin of the American Meteorological Society |
Volume | 105 |
Issue number | 7 |
DOIs | |
State | Published - Jul 2024 |
All Science Journal Classification (ASJC) codes
- Atmospheric Science