Transformation of Bottom Pressure Generated by Sea Wind Waves into Micro-Displacements of the Upper Layer of the Earth's Crust

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Resumo

A quantitative assessment of the relationship between variations in bottom pressure created by wind waves and micro-displacements of the upper crust layer is given based on data from a laser hydrosphere pressure variation meter and two laser strainmeters. Based on experimental data, the dependence of the coefficient of transformation of bottom pressure into elastic oscillations of the upper crust layer on periods of wind waves is derived.

Sobre autores

G. Dolgikh

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia

V. Antonov

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Email: antonov.va@poi.dvo.ru
Vladivostok, Russia

S. Budrin

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia

S. Dolgikh

V.I. Il’ichev Pacific Oceanological Institute, Far Eastern Branch of the Russian Academy of Sciences; Institute of Automation and Control Processes, Far Eastern Branch of the Russian Academy of Sciences

Vladivostok, Russia; Vladivostok, Russia

Bibliografia

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