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Transformations of Bottom Pressure Variations Generated by Marine Infragravity Waves into Displacements of the Upper Layer of the Earth’s Crust: Quantitative Assessment

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Abstract

Transformations of bottom pressure variations generated by infragravity waves into displacements of the upper layer of the Earth’s crust have been quantitatively assessed based on the experimental data obtained with a laser meter for hydrospheric pressure variations and two laser strainmeters. The relationship between the coefficient of bottom pressure transformation into elastic vibrations of the Earth’s crust and the infragravity wave period has been determined.

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Funding

This work was supported in part by the Russian Science Foundation (project no. 22-27-00678 “Microdeformations of the Earth’s Crust Caused by Infragravity Sea Waves According to the Laser Interference Device Data”).

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Authors and Affiliations

  1. Il’ichev Pacific Oceanological Institute, Far East Branch, Russian Academy of Sciences, 690041, Vladivostok, Russia

    G. I. Dolgikh, S. S. Budrin & S. G. Dolgikh

Authors
  1. G. I. Dolgikh
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  2. S. S. Budrin
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  3. S. G. Dolgikh
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Corresponding author

Correspondence to S. S. Budrin.

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The authors of this work declare that they have no conflicts of interest.

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Translated by E. Maslennikova

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Dolgikh, G.I., Budrin, S.S. & Dolgikh, S.G. Transformations of Bottom Pressure Variations Generated by Marine Infragravity Waves into Displacements of the Upper Layer of the Earth’s Crust: Quantitative Assessment. Dokl. Earth Sc. (2024). https://doi.org/10.1134/S1028334X24600841

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  • DOI: https://doi.org/10.1134/S1028334X24600841

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