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- W4307702373 abstract "The air-sea drag coefficient ( C d ) is closely related to tropical cyclone (TC) intensification. Several recent studies suggested that the C d decreases in winds greater than 33 m s −1 . The effects of C d reduction in high winds on TC intensity, especially rapid intensification (RI) and the lifetime maximum intensity (LMI) distribution, were investigated by analyzing the wind-dependent C d -based ocean vertical mixing and the energy budget. In addition, to consider the uncertainty of the Cd in extreme winds (above 50 m s −1 ), three types of C d fitting that decrease after 33 m s −1 , which show different trends after 50 m s −1 (increase, flat, and decrease), were adopted. The results were then compared with those for the control fitting (saturated after 33 m s −1 ) and show that the reduced C d in high winds drives an increase in net energy by reducing frictional dissipation and suppressing sea surface cooling. This extra energy prevents the TC from achieving a steady-state, causing the bimodality of simulated maximum potential intensity. The observed steady-state probability (intensification rate and RI probability) in the C d reduced wind range were significantly lower (higher) than in the others. These results suggest that C d reduction might potentially induce the RI and LMI bimodality." @default.
- W4307702373 created "2022-11-05" @default.
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- W4307702373 date "2022-10-28" @default.
- W4307702373 modified "2023-10-18" @default.
- W4307702373 title "Effects of the reduced air-sea drag coefficient in high winds on the rapid intensification of tropical cyclones and bimodality of the lifetime maximum intensity" @default.
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- W4307702373 doi "https://doi.org/10.3389/fmars.2022.1032888" @default.
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