양자강 담수의 황해와 동중국해 수온상승 효과

DC Field Value Language
dc.contributor.author 박태욱 -
dc.contributor.author 장찬주 -
dc.contributor.author 박원선 -
dc.contributor.author 오임상 -
dc.date.accessioned 2020-07-16T15:50:53Z -
dc.date.available 2020-07-16T15:50:53Z -
dc.date.created 2020-02-11 -
dc.date.issued 2011-06-02 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/28356 -
dc.description.abstract This study explores the effects of the Changjiang river discharge (CRD) on the density stratifications and associated sea surface temperature (SST) changes using a global ocean general circulation model with regional focus on the Yellow and East China Seas (YECS). The regressed field of SST on the CRD and cyclostationary EOF analysis find that the CRD contributes to maintaining warm sea surface in August. This warming is attributable to the formation of CRD-induced barrier layer, which tends to enhance stratification at the mixed layer base, thereby reducing both vertical mixing and entrainment cooling. The SST difference between the composites of flood and drought years confirms that the surface warming is related to surface freshening by the CRD. This result suggests that the CRD-induced barrier layer is an important contributor to the surface heat budget in the YECS in summer. -
dc.description.uri 2 -
dc.language English -
dc.publisher 한국해양과학기술협의회 -
dc.relation.isPartOf 한국해양과학기술협의회 공동학술대회 -
dc.title 양자강 담수의 황해와 동중국해 수온상승 효과 -
dc.title.alternative Effects of the Changjiang freshwater on sea surface warming in the Yellow and East China Seas -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 119 -
dc.citation.startPage 116 -
dc.citation.title 한국해양과학기술협의회 공동학술대회 -
dc.identifier.bibliographicCitation 한국해양과학기술협의회 공동학술대회, pp.116 - 119 -
dc.description.journalClass 2 -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 2. Conference Papers
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