이산적 모델을 이용한 열염분순환의 장주기 변동 구조 연구

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dc.contributor.author 박영규 -
dc.date.accessioned 2020-07-17T05:30:15Z -
dc.date.available 2020-07-17T05:30:15Z -
dc.date.created 2020-02-11 -
dc.date.issued 2006-11-23 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/30731 -
dc.description.abstract From idealized numerical experiments with a depth level coordinate ocean circulation model (GFDL MOM3), the structure of interdecadal variability from thermally driven circulations has been investigated. temperature and velocity anomalies circulate cyclonically in high latitudes mainly due to interactions among temperature gradient anomalies, the subsequent velocity anomalies, and the continents that block the velocity anomalies over the northeastern corner. A phase lag between the meridional temperature gradient and overturning circulation is established as a consequence of the variability. -
dc.description.uri 2 -
dc.language English -
dc.publisher 한국기후변하협의체 -
dc.relation.isPartOf 제 4차 기흐변화학술대회 -
dc.title 이산적 모델을 이용한 열염분순환의 장주기 변동 구조 연구 -
dc.title.alternative The dynamics of interdecadal variability from an idealized ocean model -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 100 -
dc.citation.startPage 95 -
dc.citation.title 제 4차 기흐변화학술대회 -
dc.contributor.alternativeName 박영규 -
dc.identifier.bibliographicCitation 제 4차 기흐변화학술대회, pp.95 - 100 -
dc.description.journalClass 2 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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