Please use this identifier to cite or link to this item: https://doi.org/10.1017/jfm.2022.42
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dc.titleDepth-integrated wave-current models. Part 2. Current with an arbitrary profile
dc.contributor.authorYang, Zhengtong
dc.contributor.authorLiu, Philip L-F
dc.date.accessioned2023-06-08T02:55:28Z
dc.date.available2023-06-08T02:55:28Z
dc.date.issued2022-02-15
dc.identifier.citationYang, Zhengtong, Liu, Philip L-F (2022-02-15). Depth-integrated wave-current models. Part 2. Current with an arbitrary profile. JOURNAL OF FLUID MECHANICS 936. ScholarBank@NUS Repository. https://doi.org/10.1017/jfm.2022.42
dc.identifier.issn0022-1120
dc.identifier.issn1469-7645
dc.identifier.urihttps://scholarbank.nus.edu.sg/handle/10635/241700
dc.description.abstractThe depth-integrated wave-current models developed by Yang & Liu (J. Fluid Mech., vol. 883, 2020, A4) are extended to investigate currents with an arbitrary vertical profile in the water column. In the present models, horizontal velocities are decomposed into two components. The first part deduces the prescribed current velocity when waves are absent. The second part is approximated in a polynomial form. The resulting depth-integrated wave-current models are obtained by applying the weighted residual method. In the absence of currents, the present models are identical to those in Yang & Liu (J. Fluid Mech., vol. 883, 2020, A4) and are validated with several three-dimensional (3D) benchmark laboratory experiments. A theoretical analysis is conducted to study the frequency dispersion relation of linear waves on currents with an exponential vertical profile and the results are compared with numerical solutions of the Rayleigh equation. Using the new models, validations and investigations are then conducted for periodic waves and solitary waves on currents with an arbitrary profile in one-dimensional horizontal (1DH) space. Furthermore, the new models are applied to wave-current interactions in two-dimensional horizontal (2DH) space. Two scenarios are considered: (1) wave propagation over a vortex-ring-like current and (2) obliquely incident wave propagation over a 3D sheared current on a varying bathymetry. The vertical and horizontal shear of the current have significant effects on modifying various wave properties, which are well captured by the present models. However, the time-averaged velocity under wave-current interaction shows small differences with the prescribed current velocity, except in the region between the wave trough and crest.
dc.language.isoen
dc.publisherCAMBRIDGE UNIV PRESS
dc.sourceElements
dc.subjectScience & Technology
dc.subjectTechnology
dc.subjectPhysical Sciences
dc.subjectMechanics
dc.subjectPhysics, Fluids & Plasmas
dc.subjectPhysics
dc.subjectcoastal engineering
dc.subjectsurface gravity waves
dc.subjectsolitary waves
dc.subjectVERTICALLY SHEARED CURRENT
dc.subjectFINITE-AMPLITUDE WAVES
dc.subjectSURFACE-WATER WAVES
dc.subjectSHORT GRAVITY WAVES
dc.subjectINTERNAL GENERATION
dc.subjectSOLITARY WAVES
dc.subjectBOUSSINESQ
dc.subjectREFRACTION
dc.subjectSIMULATIONS
dc.subjectSCATTERING
dc.typeArticle
dc.date.updated2023-06-06T03:49:56Z
dc.contributor.departmentCIVIL AND ENVIRONMENTAL ENGINEERING
dc.description.doi10.1017/jfm.2022.42
dc.description.sourcetitleJOURNAL OF FLUID MECHANICS
dc.description.volume936
dc.published.statePublished
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