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Infragravity waves are formed as a result of the transformation of wind waves and swell in a narrow inshore and connected with movements of bottom sediments, changes in bottom relief and other lithodynamic processes. They contribute to the destruction of the coasts, that must be taken into account for the sites of laying and the landfall of submarine pipelines, the installation of production platforms on the shelf. In addition, infragravity waves are responsible for the phenomenon of harbour oscillations in port and can lead to the destruction of ships and piers. Edge waves are closely related to wave processes in the ocean and have a great influence on the propagation of tsunami waves, the transport of sedimentary material, the formation of the shoreline and coastal relief, and finally, simply the concentration of wave energy in the shelf zone of the ocean. The monograph describes the investigations of the formation of edge and infragravity waves and their manifestations in the coastal zone on the basis of field observations performed with the participation of authors. The large specialized experiments, equipment and techniques for measuring waves in the ocean were considered. Particular attention is paid to the peculiarities of wave processes in the coastal zone and to the phenomenon of harbour oscillations in ports and harbors of the Sakhalin region, as well as the formation of rhythmic forms of coastal relief.

Investigation of the generation peculiarities of infragravity and edge waves in the coastal zone using the data of the field experiments