동해에서 38-40N선을 가로지르는 극향 물질수송

DC Field Value Language
dc.contributor.author 박영규 -
dc.contributor.author 오경희 -
dc.contributor.author 석문식 -
dc.date.accessioned 2020-07-17T06:51:58Z -
dc.date.available 2020-07-17T06:51:58Z -
dc.date.created 2020-02-11 -
dc.date.issued 2006-05-15 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/31084 -
dc.description.abstract Using geostrophic calculations with a quasi-zonal CTD section obtained between38-40°N in summer 1999, and velocity estimates at 700 m level from autonomous profiling floats (Argo floats), we investigate the structure of meridional mass and heat transports in the East Sea. In the horizontal, due to eddies and the meandering of the polar front, the flow changes its direction almost at every 100 km or so. In the vertical, although the flow becomes weaker with depth the direction of the flow does not change. The total volume transport though the CTD section is 1.6 Sv, which is significantly less than the volume transport through the Korea Strait, which is around 2.5 Sv., because the CTD section does not cover the strong and narrow current along the Japanese coast (the Near shore Branch). The meriodional mass transport due to the surface wind stress across the CTD section is less than 10% of that due to the geostrophic flow. Water colder than 10C is due to it own thermohaline circulation of about 0.9 Sv, which transports about 0.04 PW across the section. -
dc.description.uri 2 -
dc.language English -
dc.publisher 한국해양과학기술협의회 -
dc.relation.isPartOf 2006년 한국해양과학기술협의회 발표논문집 -
dc.title 동해에서 38-40N선을 가로지르는 극향 물질수송 -
dc.title.alternative Mass and Heat trasnport across 38-40N in the East Sea -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 152 -
dc.citation.startPage 149 -
dc.citation.title 2006년 한국해양과학기술협의회 발표논문집 -
dc.contributor.alternativeName 박영규 -
dc.contributor.alternativeName 오경희 -
dc.contributor.alternativeName 석문식 -
dc.identifier.bibliographicCitation 2006년 한국해양과학기술협의회 발표논문집, pp.149 - 152 -
dc.description.journalClass 2 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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