Compound marine heatwaves and tropical cyclones delay the onset of the Bay of Bengal summer monsoon

Marine heatwaves (MHWs) and tropical cyclones (TCs) are prominent extreme events in the Bay of Bengal (BoB), whose co-occurrence can amplify their impacts. This study explores the mechanisms behind compound MHW-TC events and their influence on the onset of the BoB summer monsoon (BoBSM). Our findings indicate that compound MHW-TC events initiate with increased downward shortwave radiation and Ekman downwelling during MHW formation, followed by latent heat flux release and Ekman upwelling during the TC lifecycle. The interaction between increased maximum potential intensity and steering flow during compound events results in a westward shift in TC tracks, delaying precipitation and atmospheric latent heat release in the eastern BoB. These factors, as well as the warmer sea surface temperatures in the BoB, hinder the reversal of the mid-to-upper tropospheric meridional temperature gradient, ultimately postponing BoBSM onset. These insights enhance the understanding of MHW-TC interactions and their implications for predicting BoBSM onset.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2025-05-01
DOI
https://doi.org/10.1038/s41612-025-01061-5
Citations
8
Primary Topic
Tropical and Extratropical Cyclones Research
Type
article
Field-Weighted Citation Impact
10.41

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article

Compound marine heatwaves and tropical cyclones delay the onset of the Bay of Bengal summer monsoon

Chi‐Yung Tam, Xiong Zhou, Jin‐Yi Yu, Lei Zhang et al.
8 citations
npj Climate and Atmospheric Science
Tropical and Extratropical Cyclones Research
10.41
article

Compound marine heatwaves and tropical cyclones delay the onset of the Bay of Bengal summer monsoon

Chi‐Yung Tam, Xiong Zhou, Jin‐Yi Yu, Lei Zhang, Hongzhou Xu, Karumuri Ashok, Boqi Liu, Kang Xu, Jianmai Shi, Weiqiang Wang
article en
8 citations

Abstract

Marine heatwaves (MHWs) and tropical cyclones (TCs) are prominent extreme events in the Bay of Bengal (BoB), whose co-occurrence can amplify their impacts. This study explores the mechanisms behind compound MHW-TC events and their influence on the onset of the BoB summer monsoon (BoBSM). Our findings indicate that compound MHW-TC events initiate with increased downward shortwave radiation and Ekman downwelling during MHW formation, followed by latent heat flux release and Ekman upwelling during the TC lifecycle. The interaction between increased maximum potential intensity and steering flow during compound events results in a westward shift in TC tracks, delaying precipitation and atmospheric latent heat release in the eastern BoB. These factors, as well as the warmer sea surface temperatures in the BoB, hinder the reversal of the mid-to-upper tropospheric meridional temperature gradient, ultimately postponing BoBSM onset. These insights enhance the understanding of MHW-TC interactions and their implications for predicting BoBSM onset.

npj Climate and Atmospheric ScienceVol. 8(1)
Chinese University of Hong Kong (HK), Chinese Academy of Sciences (CN), University of California, Irvine (US), University of Hyderabad (IN), Institute of Oceanology (CN), South China Sea Institute Of Oceanology (CN), Chinese Academy of Meteorological Sciences (CN), Irvine University (US), Institute of Deep-Sea Science and Engineering (CN), University of Chinese Academy of Sciences (CN), Ocean University of China (CN)
National Natural Science Foundation of China, Chinese Academy of Sciences, South China Sea Institute of Oceanology, Chinese Academy of Sciences, National Key Research and Development Program of China, Basic and Applied Basic Research Foundation of Guangdong Province
Life below water
Openalex Percentile: Top 1%
Tropical and Extratropical Cyclones Research
10.41
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