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ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Physical Oceanography
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1536014
This article is part of the Research Topic Prediction Models and Disaster Assessment of Ocean Waves, and the Coupling Effects of Ocean Waves in Various Ocean-Air Processes View all 9 articles
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Predicting tropical cycloness (TCs) rapid intensification (RI) is one of the most significant challenges. This study refines the Net Energy Gain Rate (NGR) metric to improve TC intensity predictions, focusing on uncertainties in the drag coefficient (Cd) at extreme wind speeds and the effective length scale of TC-induced momentum transfer to the ocean (Rw). Using data from the western North Pacific basin (2004-2021), we conducted sensitivity analyses with four Cd parameterizations (increasing, decreasing, constant, and control) and varied Rw from 0.5 to 4 times the radius of maximum wind (Rmax). Results indicate that Rw=1Rmax consistently yields the highest correlations coefficient between NGR and intensity change in 24-hour among all combinations, especially for strong TCs (Category 3 or higher). Among the Cd parameterizations, the scenario where Cd decreases at wind speeds exceeding 50 m s⁻¹ showed superior performance in capturing intensity changes. Multi-linear regression models incorporating NGR, prior 12-hour intensity changes, and vertical wind shear confirmed that decreasing Cd at Rw=1Rmax provides the most reliable predictions, achieving the highest prediction performance in the TC intensity change in 24-hour the highest coefficients of determination and lowest mean absolute errors. These findings underscore the importance of accurately representing Cd behavior under extreme wind conditions and precisely defining Rw to enhance the predictive skill of NGR-based TC intensity forecasts.
Keywords: drag coefficient, Tropical cyclone intensity change, Rapid intensification, Air-sea interactions, net energy gain rate
Received: 28 Nov 2024; Accepted: 03 Mar 2025.
Copyright: © 2025 Kim, Lee, Won, Kang, Kim and Kang. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Sunghun Kim, Korea Institute of Ocean Science and Technology (KIOST), Busan, Republic of Korea
Woojeong Lee, National typhoon center, Jeju, Republic of Korea
Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.
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