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Johannes M. L. Dahl aDepartment of Geosciences, Texas Tech University, Lubbock, Texas

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Christian Boyer bDepartment of Earth and Atmospheric Sciences, Central Michigan University, Mount Pleasant, Michigan

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© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author: Johannes Dahl, johannes.dahl@ttu.edu

© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).

Corresponding author: Johannes Dahl, johannes.dahl@ttu.edu
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  • Boyer, C., and J. M. L. Dahl, 2020: The mechanisms responsible for large near-surface surface vertical vorticity within supercellular and quasi-linear storm modes. Mon. Wea. Rev., 148, 42814297, https://doi.org/10.1175/MWR-D-20-0082.1.

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  • Fischer, J., and J. M. L. Dahl, 2022: Transition of near-ground vorticity dynamics during tornadogenesis. J. Atmos. Sci., 79, 467483, https://doi.org/10.1175/JAS-D-21-0181.1.

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