Kelvin wave hydraulic control induced by interactions between vortices and topography

DOI10.1017/jfm.2011.344zbMath1241.76112OpenAlexW2086653784MaRDI QIDQ2893727

W. K. Dewar, Marshall L. Ward, Andrew Mcc. Hogg, P. Berloff

Publication date: 26 June 2012

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: http://hdl.handle.net/1885/38834

zbMATH Keywords

rotating flowsgeostrophic turbulencehydraulic control

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Water waves, gravity waves; dispersion and scattering, nonlinear interaction (76B15) General theory of rotating fluids (76U05) Flow control and optimization for incompressible inviscid fluids (76B75)

Related Items (6)

Vortex–wall interaction on the β-plane and the generation of deep submesoscale cyclones by internal Kelvin Waves–current interactions ⋮ Quasi-geostrophy against the wall ⋮ Turbulent exchanges between near-inertial waves and balanced flows ⋮ The propagation and decay of a coastal vortex on a shelf ⋮ The effects of vertical mixing on nonlinear Kelvin waves ⋮ Existence and properties of ageostrophic modons and coherent tripoles in the two-layer rotating shallow water model on the -plane

Cites Work

• Ocean Circulation Kinetic Energy: Reservoirs, Sources, and Sinks
• V<scp>ERTICAL</scp> M<scp>IXING</scp>, E<scp>NERGY</scp>, <scp>AND THE</scp> G<scp>ENERAL</scp> C<scp>IRCULATION OF THE</scp> O<scp>CEANS</scp>

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