Abstract
The number of tropical cyclones (TCs) over the western North Pacific (WNP) dropped to a record low in 2023, with less than 40% forming during the boreal autumn. While a strong El Niño, positive Indian Ocean Dipole (pIOD), and strong tropical North Atlantic warming coexisted, their relative contributions to the suppressed TC genesis remain unclear. Through observational analyses and model experiments, we demonstrate that the tropical Atlantic and Pacific exerted minimal influence on TC genesis over the WNP. In contrast, the pIOD played a dominant role in suppressing TC activities over the central WNP, where the decline was most pronounced. Specifically, the pIOD induced easterly wind anomalies over the Indo-western Pacific, leading to descending anomalies over the WNP that inhibited TC genesis. Our findings highlight the importance of incorporating the IOD into future seasonal TC forecasts to improve its prediction skill. © The Author(s) 2025.
| Original language | English |
|---|---|
| Article number | 322 |
| Number of pages | 8 |
| Journal | npj Climate and Atmospheric Science |
| Volume | 8 |
| Online published | 2 Sept 2025 |
| DOIs | |
| Publication status | Published - 2025 |
Funding
This work is suppported by the National Natural Science Foundation of China (42376021), the National Key R&D Program of China: Young Scientist Program (2023YFC3108800), the National Natural Science Foundation of China (W2441014), the GuangDong Basic and Applied Basic Research Foundation (2024B1515040024), the Development fund (SCSIO202203) and Special fund (SCSIO2023QY01) of South China Sea Institute of Oceanology of the Chinese Academy of Sciences. The numerical simulations are supported by the High-Performance Computing Division in the South China Sea Institute of Oceanology.
Publisher's Copyright Statement
- This full text is made available under CC-BY-NC-ND 4.0. https://creativecommons.org/licenses/by-nc-nd/4.0/
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