동중국해에서의 저층 난류
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 장성태 | - |
dc.contributor.author | 이재학 | - |
dc.contributor.author | 홍창수 | - |
dc.contributor.author | 장찬주 | - |
dc.contributor.author | 유주형 | - |
dc.date.accessioned | 2020-07-17T06:50:22Z | - |
dc.date.available | 2020-07-17T06:50:22Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2006-05-16 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/31029 | - |
dc.description.abstract | The bottom boundary layer plays an important role on the dynamics of the ocean. The boundary layer turbulence removes kinetic energy from the mean flow and is responsible for advecting quantities such as sediments, oxygen, salt and heat. In order to investigate the behavior of the boundary layer turbulence, Korea Ocean Research and Development Institute conducted hydrographic survey and measured turbulence structure in the northern East China Sea in August 2005. The current was estimated by the bottom moored ADCP near the Ieodo Ocean Research Station. The microstructure measurements were obtained with the microstructure profiler, TurboMAP. | - |
dc.description.uri | 2 | - |
dc.language | English | - |
dc.publisher | 한국해양과학기술협의회 | - |
dc.relation.isPartOf | 2006년도 한국해양과학기술협의회 공동학술대회 | - |
dc.title | 동중국해에서의 저층 난류 | - |
dc.title.alternative | Oceanic turbulence within the bottom boundary layer in the East China Sea | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 162 | - |
dc.citation.startPage | 162 | - |
dc.citation.title | 2006년도 한국해양과학기술협의회 공동학술대회 | - |
dc.contributor.alternativeName | 장성태 | - |
dc.contributor.alternativeName | 이재학 | - |
dc.contributor.alternativeName | 홍창수 | - |
dc.contributor.alternativeName | 장찬주 | - |
dc.contributor.alternativeName | 유주형 | - |
dc.identifier.bibliographicCitation | 2006년도 한국해양과학기술협의회 공동학술대회, pp.162 | - |
dc.description.journalClass | 2 | - |