Abstract
The impacts of tropical cyclones (TCs) on Southeast Asia’s coastlines are acute due to high population densities in low-lying coastal environments. However, the trajectories of TCs are uncertain in a warming climate. Here, we assess >64,000 simulated TCs from the nineteenth century to the end of the twenty-first century for both moderate- and high-emissions scenarios. Results suggest changes to TC trajectories in Southeast Asia, including: (1) poleward shifts in both genesis and peak intensification rates; (2) TC formation and fastest intensification closer to many coastlines; (3) increased likelihoods of TCs moving most slowly over mainland Southeast Asia; and (4) TC tracks persisting longer over land. In the cities of Hai Phong (Vietnam), Yangon (Myanmar), and Bangkok (Thailand), these variations result in future increases in both peak TC intensity and TC duration compared to historical TCs. © The Author(s) 2024.
| Original language | English |
|---|---|
| Article number | 156 |
| Journal | npj Climate and Atmospheric Science |
| Volume | 7 |
| Online published | 2 Jul 2024 |
| DOIs | |
| Publication status | Published - 2024 |
| Externally published | Yes |
Funding
The authors wish to thank Kerry Emanuel (Massachusetts Institute of Technology) for the generation and use of synthetic TC datasets for this analysis. This research/project is supported by the Ministry of Education, Singapore, under its MOE Academic Research Fund #021940-00001 and Tier 3, Award MOE-MOET32022-0006. This is Earth Observatory of Singapore contribution number 574.
Publisher's Copyright Statement
- This full text is made available under CC-BY 4.0. https://creativecommons.org/licenses/by/4.0/
Policy Impact
- Cited in Policy Documents
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