Abstract
In this paper one of the kinds of the interaction between hydrophysical and seismoacoustic
fields on the ocean floor is considered. Done in natural conditions, experiments on generation of
hydroacoustic signals in the shelf region and registration seismoacoustic waves, which are exited
in the result of the interaction mentioned above by the laser strainmeters located on shore are
described. For a theoretical study of these pro-cesses method of elastodynamic Green's function
is proposed. Some results of numerical modeling are given. They show agreement with experi
ments. Thus the theory and modeling method, described in this paper, may be useful for investiga
tions of interaction in the sea-land system.
