| dc.contributor.author | John Grue | |
| dc.date.accessioned | 2022-01-30T21:17:59Z | |
| dc.date.available | 2022-01-30T21:17:59Z | |
| dc.date.issued | 9/1/2020 12:00:00 AM | |
| dc.identifier.other | %28ASCE%29WW.1943-5460.0000585.pdf | |
| dc.identifier.uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4267961 | |
| dc.description.abstract | A 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.publisher | ASCE | |
| dc.title | Mini-Tsunami Made by Ship Moving Across a Depth Change | |
| dc.type | Journal Paper | |
| dc.journal.volume | 146 | |
| dc.journal.issue | 5 | |
| dc.journal.title | Journal of Waterway, Port, Coastal, and Ocean Engineering | |
| dc.identifier.doi | 10.1061/(ASCE)WW.1943-5460.0000585 | |
| dc.page | 8 | |
| dc.tree | Journal of Waterway, Port, Coastal, and Ocean Engineering:;2020:;Volume ( 146 ):;issue: 005 | |
| dc.contenttype | Fulltext | |