Transformation of Bottom Pressure Generated by Sea Wind Waves into Microdisplacements of the Upper Layer of the Earth’s Crust

A quantitative assessment is given of the relationship between variations in bottom pressure created by wind waves and microdisplacements of the upper crust layer based on data from a laser hydrosphere pressure variation meter and two laser strain meters. 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.