Annotation
A possible physical mechanism that can help transportation of deep waters to the ocean surface in the case of a submarine earthquake is shown to be formation of a nonlinear flow generated by fluctuations of part of the ocean floor.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
M.A. Nosov, S.N. Skachko
Department of Marine and Inland Water Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Marine and Inland Water Physics, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Science News of the Faculty of Physics, Lomonosov Moscow State University
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