Transport by breaking internal gravity waves on slopes. (18th January 2016)

• Record Type: Journal Article
• Authors: Arthur, Robert S.; Fringer, Oliver B.
• Is Part Of: Journal of fluid mechanics. Volume 789(2016:Feb.)
• Page Start: 93
• Page End: 126
• Publication Date: 2016-01-18
• Subjects: internal waves, -- stratified flows, -- topographic effects; Fluid mechanics -- Periodicals; 532.005
• DOI: 10.1017/jfm.2015.723
• Languages: English
• ISSNs: 0022-1120

Abstract

Abstract : We use the results of a direct numerical simulation (DNS) with a particle-tracking model to investigate three-dimensional transport by breaking internal gravity waves on slopes. Onshore transport occurs within an upslope surge of dense fluid after breaking. Offshore transport occurs due to an intrusion of mixed fluid that propagates offshore and resembles an intermediate nepheloid layer (INL). Entrainment of particles into the INL is related to irreversible mixing of the density field during wave breaking. Maximum onshore and offshore transport are calculated as a function of initial particle position, and can be of the order of the initial wave length scale for particles initialized within the breaking region. An effective cross-shore dispersion coefficient is also calculated, and is roughly three orders of magnitude larger than the molecular diffusivity within the breaking region. Particles are transported laterally due to turbulence that develops during wave breaking, and this lateral spreading is quantified with a lateral turbulent diffusivity. Lateral turbulent diffusivity values calculated using particles are elevated by more than one order of magnitude above the molecular diffusivity, and are shown to agree well with turbulent diffusivities estimated using a generic length scale turbulence closure model. Based on a favourable comparison of DNS results with those of a similar two-dimensional case, we use two-dimensional simulations to extend our cross-shore transport results to additional wave amplitude and bathymetric slope conditions.