지난 최대 빙하기 동안 북태평양의 순환과 특성 변화 연구

DC Field Value Language
dc.contributor.author 김성중 -
dc.contributor.author 박영규 -
dc.date.accessioned 2020-07-17T03:50:11Z -
dc.date.available 2020-07-17T03:50:11Z -
dc.date.created 2020-02-11 -
dc.date.issued 2007-07-09 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/30426 -
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.description.uri 1 -
dc.language English -
dc.publisher 부산대학교 -
dc.relation.isPartOf Korean-Japan Jointed Workshop on Paleoceanography of the Bering Sea -
dc.title 지난 최대 빙하기 동안 북태평양의 순환과 특성 변화 연구 -
dc.title.alternative Circulation and Property Changes in the North Pacific Ocean for the Last Glacial Maximum -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 35 -
dc.citation.startPage 29 -
dc.citation.title Korean-Japan Jointed Workshop on Paleoceanography of the Bering Sea -
dc.contributor.alternativeName 박영규 -
dc.identifier.bibliographicCitation Korean-Japan Jointed Workshop on Paleoceanography of the Bering Sea, pp.29 - 35 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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