BOTTOM SHEAR STRESS UNDER WAVE-CURRENT INTERACTION SCIE SCOPUS

DC Field Value Language
dc.contributor.author Liang Bing-chen -
dc.contributor.author Li Hua-jun -
dc.contributor.author Lee Dong-yong -
dc.date.accessioned 2020-04-20T10:55:35Z -
dc.date.available 2020-04-20T10:55:35Z -
dc.date.created 2020-01-28 -
dc.date.issued 2008-02 -
dc.identifier.issn 1001-6058 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/4549 -
dc.description.abstract The present work adopts the COHERENS-SWAN model developed by the first author through coupling three-dimensional hydrodynamic model (COHERENS) and third-generation wave model (SWAN). Inside the COHERENS-SWAN, the SWAN is regarded as a subroutine and the time- and space-varying current velocity and surface elevation are obtained from the COHERENS. Wave-enhanced bottom shear stress, wave induced surface mixing length and wave dependent surface drag coefficient have been introduced into the COHERENS. Secondly, as wave-enhanced bottom shear stress ("bottom shear stress" described as BSS sometimes in this article) is concerned, a modified bottom shear stress Grant and Madsen model which introduces random wave field is given and introduced to COHERENS-SWAN. COHERENS-SWAN is also adopted to simulate three-dimensional flow in the Yellow River Delta with wave-current co-existing. Four numerical experiments were given to study the effects of wave-current interaction on enhancing bottom shear stress. The simulated current velocities, wave height and wave period match well with field measurement data. The simulated significant wave height and wave period for the case with considering the effects of current can give better agreement with measurement data than the case without involving the effects of current. The introduction of random wave generates lower the bottom shear stress than the case without introducing it. There are obvious differences between bottom shear stress of two way interaction and one way interaction. Velocity field obtained by the COHERENS-SWAN is reasonable according to previous studies and measurements. -
dc.description.uri 1 -
dc.language English -
dc.publisher ELSEVIER SCIENCE INC -
dc.subject WIND-DRIVEN CIRCULATION -
dc.subject SURFACE -
dc.subject MODEL -
dc.subject SEA -
dc.title BOTTOM SHEAR STRESS UNDER WAVE-CURRENT INTERACTION -
dc.type Article -
dc.citation.endPage 95 -
dc.citation.startPage 88 -
dc.citation.title JOURNAL OF HYDRODYNAMICS -
dc.citation.volume 20 -
dc.citation.number 1 -
dc.contributor.alternativeName 이동영 -
dc.identifier.bibliographicCitation JOURNAL OF HYDRODYNAMICS, v.20, no.1, pp.88 - 95 -
dc.identifier.doi 10.1016/S1001-6058(08)60032-3 -
dc.identifier.scopusid 2-s2.0-40149093369 -
dc.identifier.wosid 000261328400013 -
dc.type.docType Article -
dc.description.journalClass 1 -
dc.subject.keywordPlus WIND-DRIVEN CIRCULATION -
dc.subject.keywordPlus SURFACE -
dc.subject.keywordPlus MODEL -
dc.subject.keywordPlus SEA -
dc.subject.keywordAuthor Yellow River Delta -
dc.subject.keywordAuthor COHERENS -
dc.subject.keywordAuthor SWAN -
dc.subject.keywordAuthor wave-current interaction -
dc.subject.keywordAuthor bottom shear stress -
dc.relation.journalWebOfScienceCategory Mechanics -
dc.description.journalRegisteredClass scie -
dc.description.journalRegisteredClass scopus -
dc.relation.journalResearchArea Mechanics -
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