Response of a tropical cyclone to a subsurface ocean eddy and the role of boundary layer dynamics

We analyse a tropical cyclone simulated for a realistic ocean‐eddy field using the global, nonhydrostatic, fully coupled atmosphere–ocean ICOsahedral Nonhydrostatic (ICON) model. After intensifying rapidly, the tropical cyclone decays following its interaction with a cold wake and subsequently reint...

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Bibliographic Details
Published inQuarterly journal of the Royal Meteorological Society Vol. 148; no. 742; pp. 378 - 402
Main Authors Kumar, Arjun U., Brüggemann, Nils, Smith, Roger K., Marotzke, Jochem
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.01.2022
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