Comments on “Thermodynamic Characteristics of Downdrafts in Tropical Cyclones as Seen in Idealized Simulations of Different Intensities”

Roger K. Smith aMeteorological Institute, Ludwig-Maximilians University of Munich, Munich, Germany

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Michael T. Montgomery bDepartment of Meteorology, Naval Postgraduate School, Monterey, California

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© 2022 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: Roger K. Smith, roger.smith@lmu.de

© 2022 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: Roger K. Smith, roger.smith@lmu.de
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  • Barnes, G. M., 2008: Atypical thermodynamic profiles in hurricanes. Mon. Wea. Rev., 136, 631643, https://doi.org/10.1175/2007MWR2033.1.

  • Bryan, G. H., and R. Rotunno, 2009: The influence of near-surface, high entropy air in hurricane eyes on maximum hurricane intensity. J. Atmos. Sci., 66, 148158, https://doi.org/10.1175/2008JAS2707.1.

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  • Kilroy, G., R. K. Smith, and M. T. Montgomery, 2016: Why do model tropical cyclones grow progressively in size and decay in intensity after reaching maturity? J. Atmos. Sci., 73, 487503, https://doi.org/10.1175/JAS-D-15-0157.1.

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  • Montgomery, M. T., and R. K. Smith, 2017: Recent developments in the fluid dynamics of tropical cyclones. Annu. Rev. Fluid Mech., 49, 541574, https://doi.org/10.1146/annurev-fluid-010816-060022.

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  • Smith, R. K., and S. Vogl, 2008: A simple model of the hurricane boundary layer revisited. Quart. J. Roy. Meteor. Soc., 134, 337351, https://doi.org/10.1002/qj.216.

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  • Smith, R. K., and S. Wang, 2018: Axisymmetric balance dynamics of tropical cyclone intensification: Diabatic heating versus surface friction. Quart. J. Roy. Meteor. Soc., 144, 23502357, https://doi.org/10.1002/qj.3389.

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  • Smith, R. K., and M. T. Montgomery, 2022: Effective buoyancy and CAPE: Some implications for tropical cyclones. Quart. J. Roy. Meteor. Soc., https://doi.org/10.1002/qj.4294, in press.

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  • Smith, R. K., M. T. Montgomery, and S. Vogl, 2008: A critique of Emanuel’s hurricane model and potential intensity theory. Quart. J. Roy. Meteor. Soc., 134, 551561, https://doi.org/10.1002/qj.241.

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  • Smith, R. K., M. T. Montgomery, and S. V. Nguyen, 2009: Tropical cyclone spin up revisited. Quart. J. Roy. Meteor. Soc., 135, 13211335, https://doi.org/10.1002/qj.428.

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  • Smith, R. K., G. Kilroy, and M. T. Montgomery, 2021: Tropical cyclone life cycle in a three-dimensional numerical simulation. Quart. J. Roy. Meteor. Soc., 147, 33733393, https://doi.org/10.1002/qj.4133.

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  • Wadler, J. B., D. S. Nolan, J. A. Zhang, and L. K. Shay, 2021a: Thermodynamic characteristics of downdrafts in tropical cyclones as seen in idealized simulations of different intensities. J. Atmos. Sci., 79, 35033524, https://doi.org/10.1175/JAS-D-21-0006.1.

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  • Wadler, J. B., J. A. Zhang, R. F. Rogers, B. Jaimes, and L. K. Shay, 2021b: The rapid intensification of Hurricane Michael (2018): Storm structure and the relationship to environmental and air–sea interactions. Mon. Wea. Rev., 149, 245267, https://doi.org/10.1175/MWR-D-20-0145.1.

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