장강담수가 황동중국해 여름 해면수온 상승에 미치는 영향
DC Field | Value | Language |
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dc.contributor.author | 장찬주 | - |
dc.contributor.author | 박태욱 | - |
dc.date.accessioned | 2020-07-16T14:31:02Z | - |
dc.date.available | 2020-07-16T14:31:02Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2011-11-10 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/28056 | - |
dc.description.abstract | This study explores the effects of the Changjiang (also called the Yangtze River) 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). It is found that the CRD increases the SST in summer through a barrier layer (BL) formation that tends to enhance stratification at the mixed layer base, and thus reduces both vertical mixing and entrainment. This process is effective, particularly in August, after the CRD reaches its maximum in July. 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 BL induced by the CRD is an important contributor to the surface heat budget in the YECS. | - |
dc.description.uri | 1 | - |
dc.language | English | - |
dc.publisher | IUGG | - |
dc.relation.isPartOf | IUGG 2011 | - |
dc.title | 장강담수가 황동중국해 여름 해면수온 상승에 미치는 영향 | - |
dc.title.alternative | Contribution of the Changjiang river discharge to sea surface warming in the Yellow and East China Seas in summer | - |
dc.type | Conference | - |
dc.citation.endPage | 1 | - |
dc.citation.startPage | 1 | - |
dc.citation.title | IUGG 2011 | - |
dc.contributor.alternativeName | 장찬주 | - |
dc.contributor.alternativeName | 박태욱 | - |
dc.identifier.bibliographicCitation | IUGG 2011, pp.1 | - |
dc.description.journalClass | 1 | - |