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Observation of very large and steep internal waves of elevation near the Massachusetts coast

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dc.contributor.author Scotti, Alberto
dc.contributor.author Pineda, Jesus
dc.date.accessioned 2010-04-26T15:33:59Z
dc.date.available 2010-04-26T15:33:59Z
dc.date.issued 2004-11-25
dc.identifier.citation Geophysical Research Letters 31 (2004): L22307 en_US
dc.identifier.uri http://hdl.handle.net/1912/3314
dc.description Author Posting. © American Geophysical Union, 2004. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 31 (2004): L22307, doi:10.1029/2004GL021052. en_US
dc.description.abstract We report on near-bottom waves of elevation with amplitude nearly half the 25 m water column, very steep, and propagating into a sheared turbulent wave-guide. The waves contained trapped cores transporting parcels of water shoreward. These large waves depart strongly from weakly-nonlinear and weakly-nonhydrostatic conditions and challenge established paradigms. They can also represent an important factor in the across-shore transport of plankton and contaminants. en_US
dc.description.sponsorship Funding provided by ONR, grants N00014-01-1-0172 and N00014-03-1-0553. en_US
dc.format.mimetype application/pdf
dc.language.iso en_US en_US
dc.publisher American Geophysical Union en_US
dc.relation.uri http://dx.doi.org/10.1029/2004GL021052
dc.title Observation of very large and steep internal waves of elevation near the Massachusetts coast en_US
dc.type Article en_US
dc.identifier.doi 10.1029/2004GL021052


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