하계 동중국해에서의 혼합

DC Field Value Language
dc.contributor.author 이재학 -
dc.contributor.author 장성태 -
dc.contributor.author 홍창수 -
dc.date.accessioned 2020-07-17T00:51:56Z -
dc.date.available 2020-07-17T00:51:56Z -
dc.date.created 2020-02-11 -
dc.date.issued 2008-06-18 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/29888 -
dc.description.abstract In order to investigate the mixing of sea waters on the continental shelf in the northern East China Sea, Korea Ocean Research and Development Institute conducted hydrographic surveys including turbulence measurements using the R/V Eardo in August 2005 and August 2006. The turbulent kinetic energy dissipation rates based on velocity shear measurements are estimated to be , , and in the surface layer, bottom layer, and lower thermocline, respectively. The data sets suggest that surface layer water is being constantly mixed by winds. High dissipation rate in the lower thermocline seems to be caused by internal waves. The bottom layer with high dissipation rate also shows high turbidity, indicating the effect of tidal stirring turbulence. The vertical eddy diffusivities are near the bottom, and these high values appear to arise from both the low stability and high turbulent mixing. -
dc.description.uri 1 -
dc.language English -
dc.publisher AOGS -
dc.relation.isPartOf 5th AOGS annual meeting -
dc.title 하계 동중국해에서의 혼합 -
dc.title.alternative Mixing of sea waters in the Northern East China Sea in Summer -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 1 -
dc.citation.startPage 1 -
dc.citation.title 5th AOGS annual meeting -
dc.contributor.alternativeName 이재학 -
dc.contributor.alternativeName 장성태 -
dc.contributor.alternativeName 홍창수 -
dc.identifier.bibliographicCitation 5th AOGS annual meeting, pp.1 -
dc.description.journalClass 1 -
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