해운대 해역의 파랑 및 흐름 분석 OTHER

DC Field Value Language
dc.contributor.author 임학수 -
dc.date.accessioned 2020-04-19T23:39:39Z -
dc.date.available 2020-04-19T23:39:39Z -
dc.date.created 2020-02-10 -
dc.date.issued 2016-06 -
dc.identifier.issn 2288-7903 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/1475 -
dc.description.abstract To prevent the beach erosion and to support the beach restoration project in Haeundae, the Korean government initiated R&D project, the development of coastal erosion control technology since 2013. As a part of this project, waves and currents have been observed by AWACs in the nearshore and offshore of the Haeundae beach continuously for more than two years, to understand the processes of coastal waters and sediment transport in Haeundae. The variations of residual current and wave were estimated analysing two-year-long AWAC data measured at the mean water depth of 22 m and other short term data obtained near the surf zone of the Haeundae beach, respectively, during summer and winter. IOS T_TIDE and the moving average method for the current data over a fortnightly period (MSf) were applied for estimating the speed and direction of wave-induced current and residual current. A numerical simulation using a wave and current coupled model (ROMS-SWAN) considering wave-tide interaction in Haeundae coastal waters was also conducted for determining the wave-induced current during summer and winter seasonal swell waves (Hs : 2.5 m, Tp: 12 s), for better understanding of the coastal process near the beach. By comparing the measured data and simulated result, we found that cross-shore current during summer season is mainly caused by the eddy produced by the wave-induced current near the beach, which in turn, is generated by the strong waves coming from the S and SSW directions. During other seasons, longshore wave-induced current is produced by the swell waves coming from the E and ESE directions. The wave-induced current also generates longshore current heading west toward Dong-Back Island, west end of the beach, during all the seasons and eddy current toward Mipo-Port, east end of the beach, in summer which is well matched with the estimated residual current. In this study, we especially show the circulation patterns derived from nearshore wave-induced current and offshore residual current causing beach erosion and sediment transport in Haeundae coastal waters. -
dc.description.uri 2 -
dc.language Korean -
dc.publisher (사)한국연안방재학회 -
dc.title 해운대 해역의 파랑 및 흐름 분석 -
dc.title.alternative Analysis of Wave and Current in Haeundae Coastal Waters -
dc.type Article -
dc.citation.endPage 66 -
dc.citation.startPage 59 -
dc.citation.title 한국연안방재학회지 -
dc.citation.volume 3 -
dc.citation.number 2 -
dc.contributor.alternativeName 임학수 -
dc.identifier.bibliographicCitation 한국연안방재학회지, v.3, no.2, pp.59 - 66 -
dc.identifier.doi 10.20481/kscdp.2016.3.2.59 -
dc.identifier.kciid ART002282683 -
dc.description.journalClass 2 -
dc.description.isOpenAccess N -
dc.subject.keywordAuthor Haeundae circulation -
dc.subject.keywordAuthor residual current -
dc.subject.keywordAuthor wave-induced current -
dc.subject.keywordAuthor beach erosion -
dc.subject.keywordAuthor sediment transport -
dc.description.journalRegisteredClass other -
Appears in Collections:
Sea Power Enhancement Research Division > Coastal Disaster & Safety Research Department > 1. Journal Articles
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