Surface Current Response to Wind and Plumes in a Bay-shape Estuary of the eastern Yellow Sea: Ocean Radar Observation SCIE SCOPUS KCI

DC Field Value Language
dc.contributor.author Lee, Sang-Ho -
dc.contributor.author Kang, Chan-Young -
dc.contributor.author Choi, Byoung-Ju -
dc.contributor.author Kim, Chang-Shik -
dc.date.accessioned 2020-04-20T05:55:16Z -
dc.date.available 2020-04-20T05:55:16Z -
dc.date.created 2020-01-28 -
dc.date.issued 2013-03 -
dc.identifier.issn 1738-5261 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/3260 -
dc.description.abstract Response of surface subtidal current to wind and outflow plume in the bay-shape estuary, which had been artificially made by the Samangeum reclamation dike with two sluices in the west coast of Korea, was examined using the ocean radar-derived current data obtained in the summer 2010. The southerly wind was dominant due to Asian summer monsoon and the outflow plume water was discharged by the gate operation of the Shinsi and Garyeok sluices separated by 11 km into the study area that are opened in a southwestward direction. The monthly-mean flow pattern consisted of the westward outflow currents around the two sluices, the along-dike currents between the two sluices and the northward currents in the outer bay. Based upon the complex correlations of subtidal current to wind and outflow jets we explained that the northward mean current in the outer bay be formed by both the southerly wind-driven current and the geostrophic current by mean pressure setup due to the Ekman transport and plume water accumulation in the inner bay, and the along-dike mean current may be induced by the southerly wind that generates on-dike currents in the central region of study area and leads to pressure setup toward the dike between the two sluices. Combination of outflow jets, wind and coastline configuration affects variations of subtidal surface current in the inner bay. Variability of subtidal current in the outer bay is dominated by wind variation. The southerly wind produced the northward current in the outer bay though the outflow plumes from the two sluices turned clockwise from the inner to the outer bay due to the geostrophic balance when the wind was calm. The wind factor was from 2% to 7% depending on the amount of freshwater outflow and wind speed. Occasionally, when plume water discharges were large and the southerly wind was stronger than 5 m/s, a large eddy with a closed loop current was produced off the Shinsi sluice. -
dc.description.uri 1 -
dc.language English -
dc.publisher KOREA OCEAN RESEARCH DEVELOPMENT INST -
dc.subject OUTFLOW -
dc.title Surface Current Response to Wind and Plumes in a Bay-shape Estuary of the eastern Yellow Sea: Ocean Radar Observation -
dc.type Article -
dc.citation.endPage 139 -
dc.citation.startPage 117 -
dc.citation.title OCEAN SCIENCE JOURNAL -
dc.citation.volume 48 -
dc.citation.number 1 -
dc.contributor.alternativeName 김창식 -
dc.identifier.bibliographicCitation OCEAN SCIENCE JOURNAL, v.48, no.1, pp.117 - 139 -
dc.identifier.doi 10.1007/s12601-013-0010-5 -
dc.identifier.scopusid 2-s2.0-84875527606 -
dc.identifier.wosid 000335399800010 -
dc.type.docType Article -
dc.identifier.kciid ART001752074 -
dc.description.journalClass 1 -
dc.subject.keywordPlus OUTFLOW -
dc.subject.keywordAuthor ocean radar-derived current -
dc.subject.keywordAuthor bay-shape estuary -
dc.subject.keywordAuthor effects of wind and outflow jet -
dc.subject.keywordAuthor coastal circulation -
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 -
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