Structure and eastward extension of the Changjiang River plume in the East China Sea SCIE

DC Field Value Language
dc.contributor.author Lie, HJ -
dc.contributor.author Cho, CH -
dc.contributor.author Lee, JH -
dc.contributor.author Lee, S -
dc.date.accessioned 2020-04-21T06:25:54Z -
dc.date.available 2020-04-21T06:25:54Z -
dc.date.created 2020-01-28 -
dc.date.issued 2003-03 -
dc.identifier.issn 0148-0227 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/5528 -
dc.description.abstract [1] The hydrographic structure and offshore extension of freshwater plume discharged from the Changjiang (also known as the Yangtze) River in the northern East China Sea were investigated by analyzing conductivity-temperature-depth (CTD) data and drifter trajectories collected during the summers of 1997 and 1998. From June to early September, when southerly winds prevail, the plume tends to move northeast in the Chinese coastal area and then separates from the coastal zone to travel eastward over 400 km offshore across the western shelf of the northern East China Sea. During other seasons, when northerly winds prevail, the plume is confined to the Chinese coast. In the summer the plume in the midshelf, confined to a thin surface layer 10 to 15 m thick, extends eastward in the form of patches of low-salinity water rather than spreading as a tongue-shaped pattern from the Changjiang mouth. The eastward movement of patches in the western shelf is primarily due to upwelling favorable southerly winds. Upon reaching the vicinity of Chejudo, an island in the middle of northern East China Sea, the patches are advected to the Korea/Tsushima Strait by either the Cheju Warm Current or a northward-flowing mean current of the Kuroshio Branch Current and then finally flow into the East/Japan Sea. -
dc.description.uri 1 -
dc.language English -
dc.publisher AMER GEOPHYSICAL UNION -
dc.title Structure and eastward extension of the Changjiang River plume in the East China Sea -
dc.type Article -
dc.citation.title JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS -
dc.citation.volume 108 -
dc.citation.number C3 -
dc.contributor.alternativeName 이흥재 -
dc.contributor.alternativeName 조철호 -
dc.contributor.alternativeName 이재학 -
dc.contributor.alternativeName 이석 -
dc.identifier.bibliographicCitation JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, v.108, no.C3 -
dc.identifier.doi 10.1029/2001JC001194 -
dc.identifier.wosid 000182197900008 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.subject.keywordPlus SOUTHEASTERN HWANGHAE -
dc.subject.keywordPlus HYDROGRAPHIC FEATURES -
dc.subject.keywordAuthor Changjiang River -
dc.subject.keywordAuthor East China Sea -
dc.subject.keywordAuthor Changjiang diluted water -
dc.subject.keywordAuthor plume structure -
dc.subject.keywordAuthor offshore extension -
dc.subject.keywordAuthor pathway -
dc.relation.journalWebOfScienceCategory Oceanography -
dc.description.journalRegisteredClass scie -
dc.relation.journalResearchArea Oceanography -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 1. Journal Articles
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