TY - JOUR
T1 - Depth-integrated wave-current models. Part 2. Current with an arbitrary profile
AU - Yang, Zhengtong
AU - Liu, Philip L.F.
N1 - Funding Information:
P.L.-F.L. would like to acknowledge support from the National University of Singapore, Cornell University and the National Research Foundation in Singapore through a research grant (NRF2018NRF-NSFC003ES-002). Z.T.Y. would like to thank the Ministry of Education in Singapore for a Ph.D. Scholarship. The work presented in this paper is a result of the research effort through Enhancing Offshore System Productivity, Integrity and Survivability in Extreme Environments (ENSURE) programme supported by A*STAR under its RIE 2020 Industry Alignment Fund (Grant No. A19F1a0104).
Publisher Copyright:
© 2022 The Author(s). Published by Cambridge University Press.
PY - 2022/4/10
Y1 - 2022/4/10
N2 - The 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.
AB - The 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.
UR - http://www.scopus.com/inward/record.url?scp=85125255116&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85125255116&partnerID=8YFLogxK
U2 - 10.1017/jfm.2022.42
DO - 10.1017/jfm.2022.42
M3 - Article
AN - SCOPUS:85125255116
SN - 0022-1120
VL - 936
JO - Journal of Fluid Mechanics
JF - Journal of Fluid Mechanics
M1 - A31
ER -