Modeling effect of intersection angle on near-bed flows for waves and currents

Citation
H. Kim et al., Modeling effect of intersection angle on near-bed flows for waves and currents, J WATERW P, 127(6), 2001, pp. 308-318
Citations number
36
Categorie Soggetti
Civil Engineering
Journal title
JOURNAL OF WATERWAY PORT COASTAL AND OCEAN ENGINEERING-ASCE
ISSN journal
0733950X → ACNP
Volume
127
Issue
6
Year of publication
2001
Pages
308 - 318
Database
ISI
SICI code
0733-950X(200111/12)127:6<308:MEOIAO>2.0.ZU;2-Y
Abstract
The flow behavior of turbulent wave boundary layers with weak currents was described using a numerical model. Horizontal velocities, shear stresses, t urbulent eddy viscosities, and apparent roughnesses were described. The num erical model is based upon the fluid continuity and momentum equations in t he vertical plane. The momentum equations retain the advection terms with v ertical orbital velocity in contrast to previous numerical models. The hori zontal velocities were calculated from the momentum equations, and the vert ical orbital velocity distribution was obtained from the continuity equatio n. The Reynolds terms were modeled by a mixing length hypothesis. The model was compared with existing models for the wave friction factor by switchin g off the advection terms and produced similar answers to two existing mode ls. Next. the model was applied to a wave-only flow case with the advection terms retained. The model reproduced the measured mass transport profile b y van Doom and Godefroy reasonably well. The model was then applied to wave -current flow cases with arbitrary intersection angles. The model results f or 0 degrees, 180 degrees, and 90 degrees agreed well with measurements by van Doom and Godefroy and van der Stel and Visser, respectively. The model produced significant differences between the following and opposing current cases for the same wave condition. The model results suggest that the wave boundary layer flows for relatively strong waves and weak currents can be accurately described by taking account of the nonlinear advection terms by means of the vertical wave orbital velocity.