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Global Observations of Rotary-with-Depth Shear Spectra

dc.contributor.authorAmy F. Waterhouse
dc.contributor.authorTyler Hennon
dc.contributor.authorEric Kunze
dc.contributor.authorJennifer A. MacKinnon
dc.contributor.authorMatthew H. Alford
dc.contributor.authorRobert Pinkel
dc.contributor.authorHarper Simmons
dc.contributor.authorCaitlin B. Whalen
dc.contributor.authorElizabeth C. Fine
dc.contributor.authorJody Klymak
dc.contributor.authorJulia M. Hummon
dc.date.accessioned2023-04-12T18:39:45Z
dc.date.available2023-04-12T18:39:45Z
dc.date.copyright2022/11/21
dc.date.issued2022
dc.identifier.otherJPO-D-22-0015.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290039
dc.description.abstractInternal waves are predominantly generated by winds, tide–topography interactions, and balanced flow–topography interactions. Observations of vertical shear of horizontal velocity (
dc.publisherAmerican Meteorological Society
dc.titleGlobal Observations of Rotary-with-Depth Shear Spectra
dc.typeJournal Paper
dc.journal.volume52
dc.journal.issue12
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-22-0015.1
dc.journal.fristpage3241
dc.journal.lastpage3258
dc.page3241–3258
dc.treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 012
dc.contenttypeFulltext


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