Topographically-induced enstrophy production/dissipation in coastal models

DOI10.1063/1.2400076zbMath1146.76552OpenAlexW1985617883MaRDI QIDQ3531821

Maurizio Brocchini, James T. Kirby, R. Briganti, E. Terrile

Publication date: 3 November 2008

Published in: Physics of Fluids (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1063/1.2400076

Mathematics Subject Classification ID

Fluid mechanics (76-XX)

Related Items

Dispersive effects on wave-current interaction and vorticity transport in nearshore flows ⋮ A dissipative point-vortex model for nearshore circulation

Cites Work

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• Surf zone currents
• Large-scale vorticity generation by breakers in shallow and deep water
• Three-dimensional dispersion of momentum in wave-induced nearshore currents
• A note on the decay of vorticity in shallow flow calculations
• On the vorticity transport due to dissipating or breaking waves in shallow-water flow
• Topographically controlled, breaking-wave-induced macrovortices. Part 1. Widely separated breakwaters
• A fully nonlinear Boussinesq model for surface waves. Part 1. Highly nonlinear unsteady waves
• Topographically controlled, breaking-wave-induced macrovortices. Part 2. Changing geometries
• Topographically controlled, breaking-wave-induced macrovortices. Part 3. The mixing features

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