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dc.contributor.authorXueli Yin
dc.contributor.authorDongliang Yuan
dc.contributor.authorXiang Li
dc.contributor.authorZheng Wang
dc.contributor.authorYao Li
dc.contributor.authorCorry Corvianawatie
dc.contributor.authorAdhitya Kusuma Wardana
dc.contributor.authorDewi Surinati
dc.contributor.authorAdi Purwandana
dc.contributor.authorMochamad Furqon Azis Ismail
dc.contributor.authorAsep Sandra Budiman
dc.contributor.authorAhmad Bayhaqi
dc.contributor.authorPraditya Avianto
dc.contributor.authorEdi Kusmanto
dc.contributor.authorPriyadi Dwi Santoso
dc.contributor.authorDirh
dc.date.accessioned2023-04-12T18:37:23Z
dc.date.available2023-04-12T18:37:23Z
dc.date.copyright2022/12/06
dc.date.issued2022
dc.identifier.otherJPO-D-22-0027.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289977
dc.description.abstractThe mean circulation and volume budgets in the upper 1200 m of the Maluku Sea are studied using multiyear current meter measurements of four moorings in the Maluku Channel and of one synchronous mooring in the Lifamatola Passage. The measurements show that the mean current in the depth range of 60–450 m is northward toward the Pacific Ocean with a mean transport of 2.07–2.60 Sv (1 Sv ≡ 10
dc.publisherAmerican Meteorological Society
dc.titleMoored Observations of the Currents and Transports of the Maluku Sea
dc.typeJournal Paper
dc.journal.volume53
dc.journal.issue1
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-22-0027.1
dc.journal.fristpage3
dc.journal.lastpage18
dc.page3–18
dc.treeJournal of Physical Oceanography:;2022:;volume( 053 ):;issue: 001
dc.contenttypeFulltext


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