The Xiamen Symposium on Marine Environmental Sciences (XMAS 2025)

ID / Created Time

39 / 2024-08-29 15:57:54

Title

An Increase in Autumn Marine Heatwaves Caused by the Indian Ocean Dipole in the Bay of Bengal

Keywords

Atmosphere-ocean interaction,Extreme events,Heat wave,Sea surface temperature,Climate variability

Track/Subject

Session 60 - Indian Ocean Dynamics, Air-sea Interaction and Biogeochemical Cycles

Status

Abstract Accepted

Author

Kunming Liang / School of Marine Sciences, Nanjing University of Information Science and Technology；Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)；Fujian Provincial Key Laboratory of Marine Physical and Geological Processes, Third Institute of Oceanography, Ministry of Natural Resources；School of Atmospheric Sciences, Key Laboratory of Tropical Atmosphere-Ocean System Ministry of Education, Sun Yat-sen University

Yun Qiu / Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai)；Fujian Provincial Key Laboratory of Marine Physical and Geological Processes, Third Institute of Oceanography, Ministry of Natural Resources；Laboratory for Regional Oceanography and Numerical Modeling, Qingdao Marine Science and Technology Center

Xinyu Lin / Fujian Provincial Key Laboratory of Marine Physical and Geological Processes, Third Institute of Oceanography, Ministry of Natural Resources

Wenshu Lin / Fujian Provincial Key Laboratory of Marine Physical and Geological Processes, Third Institute of Oceanography, Ministry of Natural Resources

Xutao Ni / Fujian Provincial Key Laboratory of Marine Physical and Geological Processes, Third Institute of Oceanography, Ministry of Natural Resources

Yijun He / School of Marine Sciences, Nanjing University of Information Science and Technology,

Abstract

This study investigates the interannual variability of marine heatwaves (MHWs) in the Bay of Bengal (BOB) associated with the Indian Ocean dipole (IOD) from 1982 to 2021. The results revealed a significant positive correlation at the 95% confidence level between the IOD and MHW days in the central bay at the peak of the IOD in autumn. During positive IOD (pIOD) events, the central bay experienced more MHW days in autumn, with an average increase of 7.4 days. The increased MHW days in the central bay could be primarily attributed to the enhanced net heat flux (TQ), which is 9.7 times the contribution of ocean dynamic processes (horizontal advection + entrainment). The reduced latent heat flux loss and enhanced shortwave radiation due to the anomalous atmospheric low-level high pressure associated with the pIOD account for 63% and 50%, respectively, of the anomalous enhanced TQ, while the longwave radiation and sensible heat flux make smaller contributions of -20% and 7%. In addition, thermocline deepening in the southwestern bay, caused by this anomalous high pressure and associated anticyclonic wind anomalies, favors the occurrence and persistence of MHWs by reducing the mixed-layer cooling rate. In addition to the influence of the IOD, El Niño–Southern Oscillation mainly affects MHWs from winter to the following summer, which confirms the result of a previous study.

Home