Characteristics and Drivers of Marine Heatwaves in 2021 Summer in East Korea Bay, Japan/East Sea

Author:

Chen Sijie1ORCID,Yao Yulong23ORCID,Feng Yuting145,Zhang Yongchui6ORCID,Xia Changshui78ORCID,Sian Kenny T. C. Lim Kam9ORCID,Dong Changming123

Affiliation:

1. School of Marine Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China

2. Southern Laboratory of Ocean Science and Engineering (Guangdong Zhuhai), Zhuhai 519082, China

3. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanography, Chinese Academy of Sciences, Guangzhou 510301, China

4. Faculty of Chemistry and Environment Science, Guangdong Ocean University, Zhanjiang 524088, China

5. Research Center for Coastal Environmental Protection and Ecological Remediation, Guangdong Ocean University, Zhanjiang 524088, China

6. College of Meteorology and Oceanography, National University of Defense Technology, Nanjing 211101, China

7. First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China

8. Laboratory for Regional Oceanography and Numerical Modeling, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China

9. School of Atmospheric Science and Remote Sensing, Wuxi University, Wuxi 214105, China

Abstract

Marine heatwaves (MHWs) are persistent, discrete, extreme high-temperature events in the ocean, which can destructively affect marine ecosystems. Using satellite remote sensing data and reanalysis data from 1982 to 2021, we find that six indices characterizing the MHWs are in a remarkable increasing trend in the Japan/East Sea (JES), which shows that the most severe MHW events take place in the East Korean Bay (EKB) in the summer of 2021. Based on this finding, the present study focuses on the characteristics and mechanisms of the MHWs in the EKB and its adjacent areas from June to August 2021. The analysis reveals that the total days and mean intensity of MHWs that occur in the EKB are 1.84 and 1.47 times more than those averaged in the JES, respectively. It is shown that mechanisms for the occurrences of the MHWs in the summer of 2021 are caused by the atmospheric high-pressure system moving to the EKB area. Other reasons also decrease the water cooling: the net positive lateral heat fluxes across open boundaries, and the weak sea surface wind over the EKB area. Other possible reasons which cause the summer MHW events in 2021 need the oceanic numerical models to further investigate the issue.

Funder

National Natural Science Foundation of China

Publisher

MDPI AG

Subject

General Earth and Planetary Sciences

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