동중국해에서의 내부파 관측
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 이재학 | - |
dc.contributor.author | I.lozovasky | - |
dc.contributor.author | 장성태 | - |
dc.contributor.author | 장찬주 | - |
dc.contributor.author | 홍창수 | - |
dc.date.accessioned | 2020-07-17T06:51:26Z | - |
dc.date.available | 2020-07-17T06:51:26Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2006-05-15 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/31068 | - |
dc.description.abstract | The data obtained form a moored Acoustic Doppler Current Profiler and thermistor chains in the northern East China Sea in August 2005 reveal rich high frequency vertical perturbations for almost entire water column and give a clear evidence of the existence of internal waves. The largest amplitude generally appears in the lower thermocline with about 10 m downward displacement in a solitary wave packet. Turbulent energy dissipation in the pycnocline exceeds 10-7 W/kg implying direct effect of internal waves on the generation of turbulence. Sea level data recorded at the Ieodo Ocean Research Station indicate that solitary internal waves occur during the ebb tidal phase. On the other hand, no significant correlation between strong wind events and the internal waves is found. | - |
dc.description.uri | 2 | - |
dc.language | English | - |
dc.publisher | 한국해양과학기술협의회 | - |
dc.relation.isPartOf | 2006년도 한국해양과학기술협의회 공동학술대회 | - |
dc.title | 동중국해에서의 내부파 관측 | - |
dc.title.alternative | Observation of Internal Waves in the East China Sea | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 161 | - |
dc.citation.startPage | 161 | - |
dc.citation.title | 2006년도 한국해양과학기술협의회 공동학술대회 | - |
dc.contributor.alternativeName | 이재학 | - |
dc.contributor.alternativeName | 장성태 | - |
dc.contributor.alternativeName | 장찬주 | - |
dc.contributor.alternativeName | 홍창수 | - |
dc.identifier.bibliographicCitation | 2006년도 한국해양과학기술협의회 공동학술대회, pp.161 | - |
dc.description.journalClass | 2 | - |