Nonlinear tidal characteristics along the Uldolmok waterway off the southwestern tip of the Korean Peninsula SCOPUS KCI

DC Field Value Language
dc.contributor.author Kang, S.K. -
dc.contributor.author Yum, K.D. -
dc.contributor.author So, J.-K. -
dc.contributor.author Song, W.-O. -
dc.date.accessioned 2020-04-21T06:40:26Z -
dc.date.available 2020-04-21T06:40:26Z -
dc.date.created 2020-01-28 -
dc.date.issued 2003 -
dc.identifier.issn 1598-141X -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/5585 -
dc.description.abstract Analyses of tidal observations and a numerical model of the M2 and M4 tides in the Uldolmok waterway located at the southwestern tip of the Korean Peninsula are described. This waterway is well known for its strong tidal flows of up to more than 10 knots at the narrowest part of the channel. Harmonic analysis of the observed water level at five tidal stations reveals dramatic changes in the amplitude and phase of the shallow water constituents at the station near the narrowest part, while survey results show a decreasing trend in local mean sea levels toward the narrow section. It was also observed that the amplitudes of semi-diurnal constituents, M2 and S2 are diminishing toward the narrowest part of the waterway. Two-dimensional numerical modeling shows that the M2 energy flux is dominated by the component coming from the eastern boundary. The M2 energy is inward from both open boundaries and is transported toward the narrow region of the channel, where it is frictionally dissipated or transferred to other constituents due to a strong non-linear advection effect. It is also shown that the M4 generation is strong around the narrow region, and the abrupt decrease in the M4 amplitude in the region is due to a cancellation of the locally generated M4 with the component propagated from open boundaries. The superposition of both propagated and generated M4 contributions also explains the discontinuity of the M4 phase lag in the region. The tide-induced residual sea level change and the regeneration effect of the M2 tide through interaction with M4 are also examined. -
dc.description.uri 1 -
dc.language Korean -
dc.publisher Korea Ocean Research and Development Institute -
dc.subject harmonic analysis -
dc.subject nonlinearity -
dc.subject sea level change -
dc.subject shallow water -
dc.subject tidal channel -
dc.subject tidal current -
dc.subject tidal modeling -
dc.subject Korean Peninsula -
dc.subject South Korea -
dc.subject Uldolmok Waterway -
dc.title Nonlinear tidal characteristics along the Uldolmok waterway off the southwestern tip of the Korean Peninsula -
dc.type Article -
dc.citation.endPage 106 -
dc.citation.startPage 89 -
dc.citation.title Ocean and Polar Research -
dc.citation.volume 25 -
dc.citation.number 1 -
dc.identifier.bibliographicCitation Ocean and Polar Research, v.25, no.1, pp.89 - 106 -
dc.identifier.doi 10.4217/OPR.2003.25.1.089 -
dc.identifier.scopusid 2-s2.0-0038608829 -
dc.type.docType Article -
dc.identifier.kciid ART000855622 -
dc.description.journalClass 1 -
dc.subject.keywordPlus harmonic analysis -
dc.subject.keywordPlus nonlinearity -
dc.subject.keywordPlus sea level change -
dc.subject.keywordPlus shallow water -
dc.subject.keywordPlus tidal channel -
dc.subject.keywordPlus tidal current -
dc.subject.keywordPlus tidal modeling -
dc.subject.keywordPlus Korean Peninsula -
dc.subject.keywordPlus South Korea -
dc.subject.keywordPlus Uldolmok Waterway -
dc.subject.keywordAuthor M4 generation -
dc.subject.keywordAuthor Nonlinear tidal phenomena -
dc.subject.keywordAuthor Numerical modeling -
dc.subject.keywordAuthor Uldolmok waterway -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 1. Journal Articles
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