동중국해에서 태풍 나리 통과후 관측된 관성진동

DC Field Value Language
dc.contributor.author 이석 -
dc.contributor.author 오경희 -
dc.contributor.author 이흥재 -
dc.contributor.author 송규민 -
dc.contributor.author 강석구 -
dc.contributor.author 조철호 -
dc.date.accessioned 2020-07-16T23:30:43Z -
dc.date.available 2020-07-16T23:30:43Z -
dc.date.created 2020-02-11 -
dc.date.issued 2009-04-27 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/29548 -
dc.description.abstract To understand temporal variation of the sea water characteristic, ADOS drifters with temperature and pressure sensors are deployed in the East. Thermal structure of upper layer in the East China Sea was affected by the typhoon Nari passing at 15th to 16th of September in 2007. After immediately the typhoon passing, we found the characteristic of inertial oscillation. While the typhoon passing, inertial wave with about 24 hours period strongly shown and the clockwise rotation component is predominant. The phase between upper and lower layer show the difference more than 90°. -
dc.description.uri 1 -
dc.language English -
dc.publisher 한국해양학회 -
dc.relation.isPartOf The 15th Pacific-Asian Marginal Seas Meeting -
dc.title 동중국해에서 태풍 나리 통과후 관측된 관성진동 -
dc.title.alternative Inertial oscillations after the Typhoon Nari passage in the East China Sea -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 150 -
dc.citation.startPage 147 -
dc.citation.title The 15th Pacific-Asian Marginal Seas Meeting -
dc.contributor.alternativeName 이석 -
dc.contributor.alternativeName 오경희 -
dc.contributor.alternativeName 이흥재 -
dc.contributor.alternativeName 송규민 -
dc.contributor.alternativeName 강석구 -
dc.contributor.alternativeName 조철호 -
dc.identifier.bibliographicCitation The 15th Pacific-Asian Marginal Seas Meeting, pp.147 - 150 -
dc.description.journalClass 1 -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 2. Conference Papers
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