Abstract
Marine heatwaves (MHWs) pose significant threats to marine ecosystems and associated services, necessitating a deeper understanding of their driving mechanism. This study examines how the intensification of the Western North Pacific Subtropical High (WNPSH) influences future summer MHW occurrences in the Indian Ocean through complex ocean-atmosphere coupling. Over two thirds of CMIP6 models project more frequent an intense strong WNPSH years by the end of the 21st century, resulting in prolonged and extreme summer MHWs in the future. Westward extension of stronger WNPSH generates pronounced anomalous anticyclonic circulation, producing easterly winds that extend into the north and equatorial Indian Ocean and oppose climatological monsoon winds. While these anomalous easterlies suppress key cooling mechanisms, such as wind driven evaporative cooling and upwelling, the westward propagating downwelling Rossby waves dynamically precondition the warming in the western Indian Ocean by deepening the thermocline. This coupled system creates sustained surface and subsurface warming extending from preceding seasons into summer. Regional differences emerge in future summer MHWs through cloud-sea surface temperature (SST) feedback mechanisms. The central and northeastern Indian Ocean experiences more extreme MHWs due to reduced cloud cover, enhanced solar radiation exposure, and suppressed evaporative cooling through positive low cloud-SST feedback. Conversely, the western Indian Ocean exhibits enhanced convection and cloud formation, moderating extreme warming through negative SST-cloud feedback, exposing the region only to strong-moderate MHWs. These findings highlight the critical role of multiseasonal, coupled ocean-atmospheric interactions in shaping future summer MHW patterns, emphasizing the enhanced vulnerability of marine ecosystems. © 2025. American Geophysical Union. All Rights Reserved.
| Original language | English |
|---|---|
| Article number | e2025JC022626 |
| Journal | Journal of Geophysical Research: Oceans |
| Volume | 130 |
| Issue number | 9 |
| Online published | 3 Sept 2025 |
| DOIs | |
| Publication status | Published - Sept 2025 |
Funding
Research funding for this project was provided by the National Natural Science Foundation of China (Grant 42192563, 42120104001) and the Hong Kong RGC General Research Fund (11300920).
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 14 Life Below Water
Research Keywords
- coral reefs
- extreme warming
- future projections
- Marine heatwaves
Publisher's Copyright Statement
- COPYRIGHT TERMS OF DEPOSITED FINAL PUBLISHED VERSION FILE: © 2025. American Geophysical Union. All Rights Reserved. Sandaruwan, J. W. N. D., Zhou, W., Collins, M., & Wang, X. (2025). Future Summertime Marine Heatwaves in the Indian Ocean in Response to Enhanced Variability of the Western North Pacific Subtropical High Under Warming Climate. Journal of Geophysical Research: Oceans, 130(9), Article e2025JC022626. https://doi.org/10.1029/2025JC022626
RGC Funding Information
- RGC-funded
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Dive into the research topics of 'Future Summertime Marine Heatwaves in the Indian Ocean in Response to Enhanced Variability of the Western North Pacific Subtropical High Under Warming Climate'. Together they form a unique fingerprint.Projects
- 1 Finished
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GRF: Decadal Variation in the Impact of the NAO and Ural Blocking on Subseasonal Variation of the East Asian Winter Monsoon
ZHANG, L. (Principal Investigator / Project Coordinator), CHAN, P. W. (Co-Investigator), CHEUNG, H. (Co-Investigator) & LUO, D. (Co-Investigator)
1/08/20 → 11/03/24
Project: Research
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