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: The dynamic pressure on the sea bottom due to a constant, rectangular pressure distribution moving at a steady speed over the calm-water surface is determined. The problem is formulated and solved within the framework of potential-flow, linear-wave theory. Numerical results are presented for one beam-to-length ratio, for various water depths, and for both subcritical and supercritical speeds. (Author)

The pressure on the sea bottom due to a moving pressure distribution / by V.J. Monacella and J.N. Newman.