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

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DC Field	Value	Language
dc.contributor.author	Kim, Seong-Joong	-
dc.contributor.author	Park, Young-Gyu	-
dc.coverage.spatial	North Pacific Ocean	-
dc.date.issued	2007	-
dc.identifier.uri	https://repository.kopri.re.kr/handle/201206/7689	-
dc.description.abstract	The 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.language	English	-
dc.title	Circulation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum	-
dc.title.alternative	지난 최대 빙하기 동안 북태평양의 순환과 특성 변화 연구	-
dc.type	Proceeding	-
dc.identifier.bibliographicCitation	Kim, Seong-Joong, Park, Young-Gyu. 2007. Circulation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum. 부산대학교. 부산대학교. 2007.07.09~.	-
dc.citation.volume	1	-
dc.citation.number	1	-
dc.citation.conferenceDate	2007.07.09~	-
dc.citation.conferenceName	부산대학교	-
dc.citation.conferencePlace	부산대학교	-
dc.description.articleClassification	Pro(FULL)국제	-
dc.subject.keyword	Coupled climate model	-
dc.subject.keyword	Last Glacial Maximum	-
dc.subject.keyword	North Pacific Ocean	-
dc.subject.keyword	NorthPacific IntermediateWater	-
dc.identifier.localId	2007-0046	-