Features of the Transformation of Hydroacoustic Waves Into Seismoacoustic Waves in the Conditions of the Deep Sea and the Sea of Intermediate Depth

During the processing of experimental data from a coastal laser strainmeter obtained at the time of generation of hydroacoustic waves at a frequency of 22 Hz at various depths of the sea, it was found that the propagation of hydroacoustic waves from the place of their generation to the place of registration of transformed seismoacoustic waves occurs according to a law close to spherical.