Intrusion of low-salinity water into the Yellow Sea Interior in 2012 SCIE SCOPUS KCI

DC Field Value Language
dc.contributor.author Oh, Kyung-Hee -
dc.contributor.author Lee, Joon-Ho -
dc.contributor.author Lee, Seok -
dc.contributor.author Pang, Ig-Chan -
dc.date.accessioned 2020-04-20T04:25:11Z -
dc.date.available 2020-04-20T04:25:11Z -
dc.date.created 2020-01-28 -
dc.date.issued 2014-12 -
dc.identifier.issn 1738-5261 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/2655 -
dc.description.abstract Abnormally low-salinity water was detected in the surface layer of the central region of the Yellow Sea in August 2012. The presence of such low-salinity water in the Yellow Sea interior has never been reported previously. To understand the origin of this low-salinity water, oceanographic and wind data were analyzed, and the circulation of the surface layer was also examined in the Yellow and East China Seas using a numerical ocean model. The results confirmed that typhoons caused the low-salinity water. Two consecutive typhoons passed from east to west across the East China Sea, around the Changjiang Bank in early August 2012. Strong easterly and southeasterly winds created by the typhoons in the Yellow and East China Seas drove the low-salinity water to the north along the coast of China and northeastward toward the central region of the Yellow Sea, respectively. Usually, the northward drifting of Changjiang Diluted Water along the coast of China ends around the Jiangsu coast, where the drifting is blocked and is turned by the offshore Eulerian residual current. Therefore, the Changjiang Diluted Water does not intrude more into the Yellow Sea interior. However, in 2012, the low-salinity water drifted up to the Shandong Peninsula along the coast of China, and formed massive low-salinity water in the Yellow Sea interior combining with the other low-salinity water extended toward the central region of the Yellow Sea directly from the Changjiang Bank. Thus, the typhoons play a key role in the appearance of abnormally low-salinity water in the Yellow Sea interior and it means that the Yellow Sea ecosystem could be significantly influenced by the Changjiang Diluted Water. -
dc.description.uri 1 -
dc.language English -
dc.publisher 한국해양과학기술원 -
dc.title Intrusion of low-salinity water into the Yellow Sea Interior in 2012 -
dc.type Article -
dc.citation.endPage 356 -
dc.citation.startPage 343 -
dc.citation.title OCEAN SCIENCE JOURNAL -
dc.citation.volume 49 -
dc.citation.number 4 -
dc.contributor.alternativeName 오경희 -
dc.contributor.alternativeName 이석 -
dc.identifier.bibliographicCitation OCEAN SCIENCE JOURNAL, v.49, no.4, pp.343 - 356 -
dc.identifier.doi 10.1007/s12601-014-0032-7 -
dc.identifier.scopusid 2-s2.0-84920553242 -
dc.identifier.wosid 000347556000002 -
dc.type.docType Article -
dc.identifier.kciid ART001937512 -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus CHANGJIANG DILUTED WATER -
dc.subject.keywordPlus EAST CHINA SEAS -
dc.subject.keywordPlus RIVER -
dc.subject.keywordPlus PLUME -
dc.subject.keywordPlus ESTUARY -
dc.subject.keywordPlus SUMMER -
dc.subject.keywordPlus MODELS -
dc.subject.keywordPlus COAST -
dc.subject.keywordAuthor low-salinity water intrusion -
dc.subject.keywordAuthor Yellow Sea -
dc.subject.keywordAuthor Changjiang Diluted Water -
dc.subject.keywordAuthor typhoon -
dc.subject.keywordAuthor easterly and southeasterly winds -
dc.relation.journalWebOfScienceCategory Marine & Freshwater Biology -
dc.relation.journalWebOfScienceCategory Oceanography -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
dc.relation.journalResearchArea Marine & Freshwater Biology -
dc.relation.journalResearchArea Oceanography -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 1. Journal Articles
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