Microseisms associated with the southwest summer monsoon recorded on the seafloor of South China Sea

• Strong monsoon-associated secondary microseisms are recorded in the South China Sea. • The microseisms occurred prior to meteorologically determined summer monsoon onset. • Ocean-bottom seismic data can be used for monsoon early detection and monitoring. As the strongest component in the worldwide ambient noise field, secondary microseisms are dominantly excited by cyclonic storms. Whether unidirectionally propagating monsoon winds can induce seismically observable microseisms remains unclear. In this study, we use broadband seismic data recorded by seven ocean-bottom seismometers (OBSs) to systematically examine the possible excitation mechanism associated with the summer monsoon 2020 in the South China Sea. Spectrograms of the OBS data reveal remarkable power characterized by two notable peaks during May 18–31 in the short-period secondary microseism band of 0.25−0.5 Hz. In this time period, a monsoon onset occurred (May 23) and no tropical cyclones were recorded either in the South China Sea or Western Pacific. Around the summer monsoon onset, wind fields are transformed from northeasterly to southwesterly, driving ocean waves to propagate northeastward and exciting secondary microseisms by interactions with opposing wave trains driven by the pre-existing northeasterlies, which corresponds to the first power peak observed during May 18–20. After the dissipation of the northeasterlies-driven swell, a cyclone associated with the monsoon developed around Taiwan produces northeasterlies and excites secondary microseisms, resulting in the second peak emerged during May 22–26. Polarization analyses indicate that the microseisms are probably amplified by wave shoaling when ocean waves passing from deep to shallow water. Overall, this study provides evidence of a causal relation between monsoon onset and secondary microseisms, highlighting the potential of collecting ocean-bottom seismic data for the early detection and monitoring of monsoons.

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Publication Details

Journal
Earth and Planetary Science Letters
Published
2024-10-13
DOI
https://doi.org/10.1016/j.epsl.2024.119064
Citations
1
Primary Topic
Seismic Waves and Analysis
Type
article
Field-Weighted Citation Impact
0.53

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article

Microseisms associated with the southwest summer monsoon recorded on the seafloor of South China Sea

Pingchuan Tan, Weiwei Ding, Jianke Fan, Jiabiao Li et al.
1 citations
Earth and Planetary Science Letters
Seismic Waves and Analysis
0.53
article

Microseisms associated with the southwest summer monsoon recorded on the seafloor of South China Sea

Pingchuan Tan, Weiwei Ding, Jianke Fan, Jiabiao Li, Shaoping Lu, Zhangju Liu, Fansheng Kong, Aiguo Ruan, Han Zhang, Yulong Zhou, Xiaodong Wei, Xiongwei Niu
article en
1 citations

Abstract

• Strong monsoon-associated secondary microseisms are recorded in the South China Sea. • The microseisms occurred prior to meteorologically determined summer monsoon onset. • Ocean-bottom seismic data can be used for monsoon early detection and monitoring. As the strongest component in the worldwide ambient noise field, secondary microseisms are dominantly excited by cyclonic storms. Whether unidirectionally propagating monsoon winds can induce seismically observable microseisms remains unclear. In this study, we use broadband seismic data recorded by seven ocean-bottom seismometers (OBSs) to systematically examine the possible excitation mechanism associated with the summer monsoon 2020 in the South China Sea. Spectrograms of the OBS data reveal remarkable power characterized by two notable peaks during May 18–31 in the short-period secondary microseism band of 0.25−0.5 Hz. In this time period, a monsoon onset occurred (May 23) and no tropical cyclones were recorded either in the South China Sea or Western Pacific. Around the summer monsoon onset, wind fields are transformed from northeasterly to southwesterly, driving ocean waves to propagate northeastward and exciting secondary microseisms by interactions with opposing wave trains driven by the pre-existing northeasterlies, which corresponds to the first power peak observed during May 18–20. After the dissipation of the northeasterlies-driven swell, a cyclone associated with the monsoon developed around Taiwan produces northeasterlies and excites secondary microseisms, resulting in the second peak emerged during May 22–26. Polarization analyses indicate that the microseisms are probably amplified by wave shoaling when ocean waves passing from deep to shallow water. Overall, this study provides evidence of a causal relation between monsoon onset and secondary microseisms, highlighting the potential of collecting ocean-bottom seismic data for the early detection and monitoring of monsoons.

Earth and Planetary Science LettersVol. 647
Sun Yat-sen University (CN), Chinese Academy of Sciences (CN), Ministry of Natural Resources (CN), Institute of Oceanology (CN), Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (CN), Second Institute of Oceanography (CN), Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (CN)
National Natural Science Foundation of China, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), National Key Research and Development Program of China, Natural Science Foundation of Zhejiang Province
Life below water
Openalex Percentile: Top 34%
Seismic Waves and Analysis
0.53
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