Efimov V. In. , Kulikov E. A. , Rabinovich A. B. , Fine Y. In. L. Hydrometeoizdat, 1985. — 280 s. The main features of wave processes in the border areas of the ocean are considered: in the zones of the shelf - the continental slope, in the equatorial regions and frontal zones. Shown, that special types of horizontally heterogeneous longwave motions are formed in these regions, which significantly determine the dynamics of these parts of the ocean , resulting in the capture and condensation of wave energy, flow meandering, Mesoscale Vortex Formation , I have a defining influence on the tsunami, tides, storm surges. For oceanologists, hydrodynamicians, specialists interested in the problem of tsunami. Foreword by .