동해에서의 최근의 비균질 해수면 상승

DC Field Value Language
dc.contributor.author 강석구 -
dc.contributor.author 조셒체르니아브스키 -
dc.contributor.author 마이크포만 -
dc.contributor.author 민홍식 -
dc.contributor.author 김철호 -
dc.contributor.author 강현우 -
dc.date.accessioned 2020-07-17T09:31:38Z -
dc.date.available 2020-07-17T09:31:38Z -
dc.date.created 2020-02-11 -
dc.date.issued 2004-12-10 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/31604 -
dc.description.abstract The recent trend of sea level rise in the East/japan Sea(EJS) is investigated using TOPEX/POSEIDON(T/P) altimetry, long-term tide gauges and thermosteric sea levels(TSL) at stations where long term temperature data are available. The T/P analysis reveals an EJS-averaged increase of about 5.7+-9.1 mm/yr over 9 years, 1992-2001, which is much larger than the global rate of 3.1+-0.4 mm/yr reported by Cabanes et al.(2001). The anomalously high increasing rate of sea level rise in the Ulleung and Yamato basins is apparently due to the large temperature anomaly pattern intensified by eddy activity, which seems to be related to decadal variaitions of heat anomaly in the Northwest Pacific Ocean. -
dc.description.uri 1 -
dc.language English -
dc.publisher 한국해양학회(물리분과) -
dc.relation.isPartOf 한국해양학회(물리분과)/International workshop on East Sea Circulation -
dc.title 동해에서의 최근의 비균질 해수면 상승 -
dc.title.alternative Inhomogeneous pattern of recent sea level rise in the East/Japan Sea -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 9 -
dc.citation.startPage 7 -
dc.citation.title 한국해양학회(물리분과)/International workshop on East Sea Circulation -
dc.contributor.alternativeName 강석구 -
dc.contributor.alternativeName 민홍식 -
dc.contributor.alternativeName 김철호 -
dc.contributor.alternativeName 강현우 -
dc.identifier.bibliographicCitation 한국해양학회(물리분과)/International workshop on East Sea Circulation, pp.7 - 9 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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