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On Geostrophic Adjustment in Sea Straits and Wide Estuaries:Theory and Laboratory Experiments. Part II—Two-Layer System
Sea Straits II—Two-Layer System Wide Estuaries
2009/2/23
A frictionless nonlinear model with allowance for motions which are far from a state of geostrophic balance is considered in order to describe the dynamics of outflows consisting of two layers of flui...
On Geostrophic Adjustment in Sea Straits and Wide Estuaries:Theory and Laboratory Experiments. Part I:One-Layer System
Sea Straits Wide Estuaries One-Layer System
2009/2/23
The dynamics of outflows from sea straits and wide estuaries are examined through a simplified frictionless model whose primary motions are not constrained to be quasi-geostrophic. The potential vorti...
Laboratory Experiments on the Merging of Nonlinear Anticyclonic Eddies
Laboratory Experiments Nonlinear Anticyclonic Eddies
2009/1/7
The mutual interaction of two isolated lenslike eddies is examined with the aid of a laboratory experiment on a rotating table. The isolated anticyclonic eddies are formed by withdrawing two cylinders...
Oceanographic implications of Laboratory Experiments on Diffusive Interfaces
Oceanographic implications Diffusive Interfaces Laboratory Experiments
2009/1/5
This paper contains a summary of the results from some laboratory and theoretical studies on the diffusive interface in double diffusive convection, paying particular attention to the recent work of F...
Convective Building of a Pycnocline:Laboratory Experiments
Convective Building ycnocline Laboratory Experiments
2008/12/3
The convective building of a pycnocline is examined using a laboratory model forced by surface fluxes of saline water at one end and fresh water at the other. A deep recirculation evolves in the tank,...
Modeling Deep Ocean Convection: Large Eddy Simulation in Comparison with Laboratory Experiments
Modeling Deep Ocean Convection Laboratory Experiments Large Eddy Simulation
2008/11/14
A large-eddy simulation model (LES) has been applied to study deep convective processes in a stratified ocean driven by the energetic cooling at the ocean surface. Closely related to a recent laborato...
Interaction of Barotropic Vortices with Coastal Topography: Laboratory Experiments and Numerical Simulations
Interaction of Barotropic Vortices with Coastal Topography: Laboratory Experiments and Numerical Simulations
2008/7/3
The interaction of a barotropic cyclonic vortex on a β plane with a strong topographic slope is studied by means of laboratory experiments and numerical simulations. In the laboratory, the vortex is p...