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The interaction of ocean surface waves produces pressure fluctuations at the seafloor capable of generating seismic waves in the solid Earth. The accepted mechanism satisfactorily explains secondary microseisms of the Rayleigh type, but it does not justify the presence of transversely polarized Love waves, nevertheless widely observed. An explanation for two-thirds of the worldwide ambient wave field has been wanting for over a century. Using numerical simulations of global-scale seismic wave propagation at unprecedented high frequency, here we explain the origin of secondary microseism Love waves. A small fraction of those is generated by boundary force-splitting at bathymetric inclines, but the majority is generated by the interaction of the seismic wave field with three-dimensional heterogeneity within the Earth. We present evidence for an ergodic model that explains observed seismic wave partitioning, a requirement for full-wave field ambient-noise tomography to account for realistic source distributions.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7703644 | PMC |
http://dx.doi.org/10.1073/pnas.2013806117 | DOI Listing |
Sci Rep
November 2024
Department of Mathematics, School of Advanced Sciences VIT - AP University, Amaravati, 522237, Andhra Pradesh, India.
Light Sci Appl
July 2024
Changchun Institute of Optics, Fine Mechanics and Physics, Chinese Academy of Sciences, Changchun, 130033, China.
The sense of light is the first sensation the human body develops. The importance of light is self-evident. However, we all know that the light we can see and perceive covers only a small section of the spectrum.
View Article and Find Full Text PDFJ Fam Issues
May 2024
University of California, Los Angeles, CA, USA.
Previous work has suggested that the drastic Khmer-Rouge-era changes to the family institution have not endured. Potentially more influential in the long term were the rapid socio-economic changes Cambodia underwent starting in the 1990s. We use four waves of the Cambodian Demographic and Health Surveys from 2000 to 2014 to document contemporary trends in marriage formation and dissolution.
View Article and Find Full Text PDFSensors (Basel)
June 2024
HCK Geophysical, 9F-3, No. 79, Section 2, Roosevelt Road, Taipei 10646, Taiwan.
This paper presents an in-depth study of the stress wave behavior propagating in a Rayleigh-Love rod with sudden cross-sectional area variations. The analytical solutions of stress waves are derived for the reflection and transmission propagation behavior at the interface of the cross-sectional area change in the rod, considering inertia and Poisson's effects on the rod material. Examples solved using the finite element method are provided to verify the correctness of the analytical results.
View Article and Find Full Text PDFSensors (Basel)
May 2024
Laboratoire de l'Intégration du Matériau au Système, University of Bordeaux, CNRS, Bordeaux INP, UMR 5218, F-33405 Talence, France.
This paper presents an extended work on the Finite Element Method (FEM) simulation of Love Wave (LW) sensors in a liquid medium. Two models are proposed to simulate the multiphysical response of the sensor. Both are extensively described in terms of principle, composition and behavior, making their applications easily reproducible by the sensor community.
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