What is it about?

Idealized simulations with the Bryan Cloud Model 1 are performed. These simulations indicate that parcels of air develop rotation via different mechanisms before and after tornadogenesis. Hence, a transition of vertical vorticity source mechanisms happens during tornadogenesis as an effect of developing vortex structure.

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Why is it important?

The study offers a unified explanation for the two types of mechanisms for near-ground vertical vorticity generation, which previously have been seen as contradicting, while in fact they both seem to be important at different stages of the tornado life-cycle. This transition could also have important implications for tornado intensity.

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This page is a summary of: Transition of Near-Ground Vorticity Dynamics during Tornadogenesis, Journal of the Atmospheric Sciences, February 2022, American Meteorological Society,
DOI: 10.1175/jas-d-21-0181.1.
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