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dc.contributor.authorDelphine Hypolite
dc.contributor.authorLeonel Romero
dc.contributor.authorJames C. McWilliams
dc.contributor.authorDaniel P. Dauhajre
dc.date.accessioned2023-04-12T18:33:12Z
dc.date.available2023-04-12T18:33:12Z
dc.date.copyright2022/12/22
dc.date.issued2022
dc.identifier.otherJPO-D-22-0126.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289867
dc.description.abstractSurface gravity wave effects on currents (WEC) cause the emergence of Langmuir cells (LCs) in a suite of high horizontal resolution (Δ
dc.publisherAmerican Meteorological Society
dc.titleLangmuir Circulations Transfer Kinetic Energy from Submesoscales and Larger Scales to Dissipative Scales
dc.typeJournal Paper
dc.journal.volume53
dc.journal.issue1
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-22-0126.1
dc.journal.fristpage253
dc.journal.lastpage268
dc.page253–268
dc.treeJournal of Physical Oceanography:;2022:;volume( 053 ):;issue: 001
dc.contenttypeFulltext


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