Bin Huang 1, Mei Xue 1,2, Zhen Guo 3,4, and Wenkai Song 1,5
1State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, China.
2Shanghai Sheshan National Geophysical Observatory, Shanghai, China.
3College of Civil Engineering, Tongji University, Shanghai, China.
4Key Laboratory of Geotechnical and Underground Engineering of the Ministry of Education, Tongji University, Shanghai, China.
5Now at Department of Earth and Planetary Sciences, The University of New Mexico, Albuquerque, NM, USA.
Abstract
Single-frequency microseisms (SFMs) have been revealed to be only generated in shallow water for decades, while some recent studies reported them in deep ocean. Using the continuous waveform data recorded by ocean bottom seismometers, we investigate the deep ocean SFMs in the northern Philippine Sea. Based on the spectrum analysis, we find that the SFMs can be detected in deep ocean and the detection is time variable. To determine the source locations of SFMs, we perform polarization analysis and calculate the cross-correlation coefficients between SFMs on vertical components and ocean wave energy spectra considering the attenuation of SFMs. Both the polarization and correlation results show that the sources nearby stations dominate the observed Rayleigh-wave SFMs though distant sources also contribute. Our investigation suggests that the SFMs can be generated in deep ocean likely by infragravity ocean waves interacting with seafloor topography, which is strengthened by strong ocean storms.
Full Article:https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2021GL097444
