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Circulation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum

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dc.contributor.authorPark, Young-Gyu-
dc.contributor.authorKim, Seong-Joong-
dc.coverage.spatialNorth Pacific Ocean-
dc.date.available2018-04-05T10:41:51Z-
dc.date.issued2007-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/7687-
dc.description.abstractThe coupled model simulates an enhanced circulation in the intermediate and upper deep layers of the northern North Pacific with LGM boundary conditions, in consistent with proxy estimates. The enhanced North Pacific circulation is mainly due to the increase in surface salinity in the Sea of Okhotsk and the Bering Sea by a reduction in freshwater input.-
dc.languageEnglish-
dc.titleCirculation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum-
dc.title.alternative지난 최대 빙하기 동안 북태평양의 순환과 특성 변화 연구-
dc.typeProceeding-
dc.identifier.bibliographicCitationPark, Young-Gyu, Kim, Seong-Joong. 2007. Circulation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum. 한국해양학회. 한국해양학회. 2007.05.31~.-
dc.citation.volume1-
dc.citation.number1-
dc.citation.conferenceDate2007.05.31~-
dc.citation.conferenceName한국해양학회-
dc.citation.conferencePlace한국해양학회-
dc.description.articleClassificationPro(FULL)국내-
dc.subject.keywordCoupled climate model-
dc.subject.keywordLast Glacial Maximum-
dc.subject.keywordNorth Pacific Ocean-
dc.subject.keywordNorthPacific IntermediateWater-
dc.identifier.localId2007-0044-
Appears in Collections  
2007-2010, Integrated research on the COMposition of Polar Atmosphere and Climate Change(COMPAC) (07-10) / Lee, Bang Yong (PE07030, PE08030, PE09030, PE10030, PG07012)
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