The westward intrusion of south Pacific water at the western tip of the New Guinea Island SCIE SCOPUS

DC Field Value Language
dc.contributor.author Kim, Eung -
dc.contributor.author Jeon, Dongchull -
dc.contributor.author Hadikusumah -
dc.date.accessioned 2020-04-20T05:55:29Z -
dc.date.available 2020-04-20T05:55:29Z -
dc.date.created 2020-01-28 -
dc.date.issued 2013-01 -
dc.identifier.issn 0253-505X -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/3285 -
dc.description.abstract Fromthe eastern Indonesian cruise from November 14 to 23, 2007, CTD (conductivity, temperature, depth profiler) /ADCP (acoustic Doppler current profiler)casting and seawater sampling were done at 25 stations around Waigeo Island near New Guinea Island. It was found overall westward intrusion of the south Pacific waters into the Seram Sea and southward spreading of the north and south Pacific waters into the Seram Sea. There is westward residual flow along the channel between Waigeo and New Guinea within upper 200 m with the maximum speed up to 50 cm/s, and much weaker eastward flow in the lower layer (< 10 cm/s) due to blocking by the shallow sill at the west of the Dampier Strait. The abrupt change of bottom topography induces active horizontal and vertical mixing which results in a three-layered current system with a major through-flow of -0.99 Sv (Sv = 10(6) m(3)/s) into the Seram Sea; the transports in the upper and the lower layers are -1.14 Sv and -0.24 Sv (westward), respectively, and in the middle there is a return flow with the transport of +0.39 Sv (eastward). -
dc.description.uri 1 -
dc.language English -
dc.publisher SPRINGER -
dc.subject EQUATORIAL PACIFIC -
dc.subject NORTH PACIFIC -
dc.subject OCEAN CIRCULATION -
dc.subject MINDANAO CURRENT -
dc.subject UNDERCURRENT -
dc.subject VARIABILITY -
dc.subject TURBULENCE -
dc.subject SECTION -
dc.title The westward intrusion of south Pacific water at the western tip of the New Guinea Island -
dc.type Article -
dc.citation.endPage 31 -
dc.citation.startPage 24 -
dc.citation.title ACTA OCEANOLOGICA SINICA -
dc.citation.volume 32 -
dc.citation.number 1 -
dc.identifier.bibliographicCitation ACTA OCEANOLOGICA SINICA, v.32, no.1, pp.24 - 31 -
dc.identifier.doi 10.1007/s13131-013-0264-x -
dc.identifier.scopusid 2-s2.0-84872393068 -
dc.identifier.wosid 000313293900003 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus EQUATORIAL PACIFIC -
dc.subject.keywordPlus NORTH PACIFIC -
dc.subject.keywordPlus OCEAN CIRCULATION -
dc.subject.keywordPlus MINDANAO CURRENT -
dc.subject.keywordPlus UNDERCURRENT -
dc.subject.keywordPlus VARIABILITY -
dc.subject.keywordPlus TURBULENCE -
dc.subject.keywordPlus SECTION -
dc.subject.keywordAuthor a three-layered system -
dc.subject.keywordAuthor New Guinea coastal undercurrent -
dc.subject.keywordAuthor south Pacific tropical water (SPTW) -
dc.subject.keywordAuthor south Pacific intermediate water (SPIW) -
dc.subject.keywordAuthor vertical mixing -
dc.relation.journalWebOfScienceCategory Oceanography -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Oceanography -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 1. Journal Articles
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