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dc.contributor.authorHua Zheng
dc.contributor.authorXiao-Hua Zhu
dc.contributor.authorChuanzheng Zhang
dc.contributor.authorRuixiang Zhao
dc.contributor.authorZe-Nan Zhu
dc.contributor.authorQiang Ren
dc.contributor.authorYansong Liu
dc.contributor.authorFeng Nan
dc.contributor.authorFei Yu
dc.date.accessioned2023-04-12T18:29:57Z
dc.date.available2023-04-12T18:29:57Z
dc.date.copyright2022/09/01
dc.date.issued2022
dc.identifier.otherJPO-D-21-0284.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4289774
dc.description.abstractSouth China Sea (SCS) abyssal circulation largely contributes to water renewal, energy budget, and sedimentary processes in the deep ocean. The three-dimensional abyssal circulation west of the Luzon Strait (LS) in the northern SCS was investigated using an array comprising 27 current- and pressure-recording inverted echo sounders. Over 400 days of measurements from June 2018 to July 2019 showed a narrow and strong (∼70 km, ∼2.3 cm s
dc.publisherAmerican Meteorological Society
dc.titleObservation of Abyssal Circulation to the West of the Luzon Strait, South China Sea
dc.typeJournal Paper
dc.journal.volume52
dc.journal.issue9
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-21-0284.1
dc.journal.fristpage2091
dc.journal.lastpage2109
dc.page2091–2109
dc.treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 009
dc.contenttypeFulltext


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