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dc.contributor.authorGregory Sinnett
dc.contributor.authorSteven R. Ramp
dc.contributor.authorYiing J. Yang
dc.contributor.authorMing-Huei Chang
dc.contributor.authorSen Jan
dc.contributor.authorKristen A. Davis
dc.date.accessioned2023-04-12T18:33:16Z
dc.date.available2023-04-12T18:33:16Z
dc.date.copyright2022/10/07
dc.date.issued2022
dc.identifier.otherJPO-D-21-0273.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289869
dc.description.abstractLarge-amplitude internal solitary wave (ISW) shoaling, breaking, and run-up was tracked continuously by a dense and rapidly sampling array spanning depths from 500 m to shore near Dongsha Atoll in the South China Sea. Incident ISW amplitudes ranged between 78 and 146 m with propagation speeds between 1.40 and 2.38 m s
dc.publisherAmerican Meteorological Society
dc.titleLarge-Amplitude Internal Wave Transformation into Shallow Water
dc.typeJournal Paper
dc.journal.volume52
dc.journal.issue10
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-21-0273.1
dc.journal.fristpage2539
dc.journal.lastpage2554
dc.page2539–2554
dc.treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 010
dc.contenttypeFulltext


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