Please use this identifier to cite or link to this item: http://ir.library.ui.edu.ng/handle/123456789/9332
Full metadata record
DC FieldValueLanguage
dc.contributor.authorBello, A. K.-
dc.contributor.authorOgunseye, T. T.-
dc.contributor.authorAdetoyinbo, A. A.-
dc.contributor.authorIbrahim, A. H.-
dc.date.accessioned2024-06-24T10:28:13Z-
dc.date.available2024-06-24T10:28:13Z-
dc.date.issued2018-07-
dc.identifier.otherui_art_bello_numerical_2018-
dc.identifier.otherJournal of the Nigerian Association of Mathematical Physics 47 pp. 111-116-
dc.identifier.urihttp://ir.library.ui.edu.ng/handle/123456789/9332-
dc.description.abstractThe numerical modeling of topographic waves is based on the continuity and momentum equations. The solutions of these equations for the vertical and horizontal velocities and surface elevation of the oceans were obtained through a FORTRAN- program that was run using different values of bottom slope (a), coefficient of bottom friction (r) at different intervals (n). Slopes of the plots of horizontal, vertical velocities and surface elevation of the ocean for flat bottom ocean and fixed values of bottom friction were obtained. Similarly, slopes of the plots of resultant velocity against surface elevation and surface elevation versus horizontal and vertical velocity were also obtained. The resultant velocity (c) against the surface elevation η of the ocean produced negative slopes. The low value of slopes is an indication that the ocean waves move slowly and steadily.en_US
dc.language.isoenen_US
dc.subjectResultant Velocityen_US
dc.subjectBottom Slopeen_US
dc.subjectBottom Friction Coefficienten_US
dc.subjectSurface Elevationen_US
dc.subjectTopographic Wavesen_US
dc.titleNumerical modeling to study the effect of small bottom irregularities on steady flow in homogeneous oceanen_US
dc.typeArticleen_US
Appears in Collections:Scholarly works

Files in This Item:
File Description SizeFormat 
(25) ui_art_bello_numerical_2018.pdf2.57 MBAdobe PDFThumbnail
View/Open


Items in UISpace are protected by copyright, with all rights reserved, unless otherwise indicated.