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dc.contributor.authorPeter P. Sullivan
dc.contributor.authorJames C. McWilliams
dc.date.accessioned2023-04-12T18:33:40Z
dc.date.available2023-04-12T18:33:40Z
dc.date.copyright2022/10/03
dc.date.issued2022
dc.identifier.otherJAS-D-22-0019.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289881
dc.description.abstractImagery and numerical modeling show an abundance of submesoscale oceanic eddies in the upper ocean. Large-eddy simulation (LES) is used to elucidate eddy impacts on the atmospheric boundary layer (ABL) forced by winds, convection, and an eddy with varying radius; the maximum azimuthal eddy speed is 1 m s
dc.publisherAmerican Meteorological Society
dc.titleAtmospheric Boundary Layers over an Oceanic Eddy
dc.typeJournal Paper
dc.journal.volume79
dc.journal.issue10
dc.journal.titleJournal of the Atmospheric Sciences
dc.identifier.doi10.1175/JAS-D-22-0019.1
dc.journal.fristpage2601
dc.journal.lastpage2620
dc.page2601–2620
dc.treeJournal of the Atmospheric Sciences:;2022:;volume( 079 ):;issue: 010
dc.contenttypeFulltext


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