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Vertical Convergence of Turbulent and Double-Diffusive Heat Flux Drives Warming and Erosion of Antarctic Winter Water in Summer

dc.contributor.authorGiddy, I. S.
dc.contributor.authorFer, I.
dc.contributor.authorSwart, S.
dc.contributor.authorNicholson, S.-A.
dc.date.accessioned2024-12-24T14:07:46Z
dc.date.available2024-12-24T14:07:46Z
dc.date.copyright01 Aug. 2023
dc.date.issued2023
dc.identifier.otherphoc-JPO-D-22-0259.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4300206
dc.languageEnglish
dc.publisherAmerican Meteorological Society
dc.titleVertical Convergence of Turbulent and Double-Diffusive Heat Flux Drives Warming and Erosion of Antarctic Winter Water in Summer
dc.typeJournal Paper
dc.journal.volume53
dc.journal.issue8
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-22-0259.1
dc.journal.fristpage1941
dc.journal.lastpage1958
dc.treeJournal of Physical Oceanography:;2023:;volume( 053 ):;issue: 008
dc.contenttypeFulltext


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