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dc.titleMultilevel finite-difference model for three-dimensional hydrodynamic circulation
dc.contributor.authorShankar, N.J.
dc.contributor.authorCheong, H.F.
dc.contributor.authorSankaranarayanan, S.
dc.identifier.citationShankar, N.J.,Cheong, H.F.,Sankaranarayanan, S. (1997-10). Multilevel finite-difference model for three-dimensional hydrodynamic circulation. Ocean Engineering 24 (9) : 785-816. ScholarBank@NUS Repository.
dc.description.abstractA three-dimensional finite-difference multilevel hydrodynamic model is developed using an explicit scheme on a staggered grid. The model has been tested against four cases, namely (i) wind-induced circulation (ii) density-driven circulation (iii) seiche oscillation in a closed basin and (iv) tide-induced circulation in a open channel. The results obtained in the present study compare well with those obtained from the corresponding analytical solutions under idealised conditions for the above four cases. The model was also tested against the case of circulation induced by wind and Coriolis force and the results obtained are compared with the results of Davies and Owen (1979). © 1997 Elsevier Science Ltd.
dc.contributor.departmentCIVIL ENGINEERING
dc.description.sourcetitleOcean Engineering
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