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  4. Suppression of marine heatwave activity by tropical cyclone–induced upper ocean cooling
 
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Suppression of marine heatwave activity by tropical cyclone–induced upper ocean cooling

Journal
Science Advances
Journal Volume
11
Journal Issue
46
ISSN
2375-2548
Date Issued
2025-11-14
Author(s)
Pun, Iam-Fei
Lin, I-I  
Wu, Chun-Chieh  
DOI
10.1126/sciadv.adw8070
URI
https://www.scopus.com/pages/publications/105021697048
https://scholars.lib.ntu.edu.tw/handle/123456789/734922
Abstract
Marine heatwaves (MHWs) have drawn substantial scientific attention due to their profound biological and economic impacts, especially in the context of climate change. This study highlights the crucial role of tropical cyclones (TCs) in disrupting MHWs by altering ocean temperatures. As demonstrated by Tropical Cyclone Bavi, intense sea surface temperature (SST) cooling, reaching up to 7°C, immediately terminated a mature MHW and suppressed subsequent MHW development for up to 8 months. More generally, on the basis of post-TC MHW cases (reoccurring within 1 month) during 2014 to 2023, we found that MHW disruption duration is proportional to the magnitude of TC-induced SST cooling, ~5 to 7 days per degree of cooling. At a broader scale, a 20-year (2004 to 2023) analysis revealed 99% significant inverse relationships between seasonal MHW and TC activity. These findings suggest that TCs can act as natural regulators, effectively mitigating heat stress from MHWs and potentially serving as a lifeline for marine ecosystems.
Subjects
adult
article
climate change
controlled study
cooling
duration
heat stress
heat wave
hurricane
male
marine environment
nonhuman
sea surface temperature
temperature
Publisher
American Association for the Advancement of Science (AAAS)
Type
journal article

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