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dc.contributor.authorJohn Grue
dc.date.accessioned2022-01-30T21:17:59Z
dc.date.available2022-01-30T21:17:59Z
dc.date.issued9/1/2020 12:00:00 AM
dc.identifier.other%28ASCE%29WW.1943-5460.0000585.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4267961
dc.description.abstractA ship moving across a shallow depth change, in water in a small or narrow space, may create a small tsunami, 0.5–1 km long, observed as a harbor wave on shore, where a wave height up to 1.4 m has been measured. The paper gives an interpretation of the generation process of this new phenomenon. At a depth change, the ship-induced fluid velocity produces a reaction velocity of equal magnitude and opposite direction, orthogonal to the bottom. This velocity appears as a vertical velocity at the water surface, making the waves. The waves propagate with the shallow water speed upstream of a ship moving at subcritical speed. Theory and numerical calculations for a real ship geometry are compared with a moving pressure distribution. Computations compare favorably with a few available wave height measurements.
dc.publisherASCE
dc.titleMini-Tsunami Made by Ship Moving Across a Depth Change
dc.typeJournal Paper
dc.journal.volume146
dc.journal.issue5
dc.journal.titleJournal of Waterway, Port, Coastal, and Ocean Engineering
dc.identifier.doi10.1061/(ASCE)WW.1943-5460.0000585
dc.page8
dc.treeJournal of Waterway, Port, Coastal, and Ocean Engineering:;2020:;Volume ( 146 ):;issue: 005
dc.contenttypeFulltext


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