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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Published in | Quarterly journal of the Royal Meteorological Society Vol. 148; no. 742; pp. 378 - 402 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Chichester, UK
John Wiley & Sons, Ltd
01.01.2022
Wiley Subscription Services, Inc |
Subjects | |
Online Access | Get full text |
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