The linear equations governing stratified, wind-driven flow in an ocean of arbitrary shape may be combined into a single advection-diffusion equation for the pressure , in which the flow advecting includes a delta-function contribution at the ocean bottom in the sense of southward advection of along western continental slopes. This interpretation of the -equation helps to explain numerical solutions obtained with a finite-element model incorporating realistic North Atlantic bathymetry
The Large-scale Semi-Geostrophic Equations (LSGE, Salmon[73]) are three-dimensional equations valid ...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...
A numerical exploration of inertial equilibrium states obtained with a primitive equation ocean mode...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
We offer a simple model for studying the joint effect of baroclinicity and relief (jebar) on large-s...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Described in this paper is a technique of using artificial water boundaries in theories of ocean cur...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
The circulation in a coastal upwelling region with a shelf area is calculated. It is assumed that th...
The quasigeostrophic, wind-driven circulation theory given by Rhines and Young (1982b) is extended i...
Using the Monte Carlo method of statistical physics, we compute the equilibrium statistical mechanic...
The tides on a regular open coast change rapidly as a stonn approaches, and the time history of this...
The nature of the steady buoyancy-driven circulation is investigated using multi-level numerical mod...
The Large-scale Semi-Geostrophic Equations (LSGE, Salmon[73]) are three-dimensional equations valid ...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...
A numerical exploration of inertial equilibrium states obtained with a primitive equation ocean mode...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
We offer a simple model for studying the joint effect of baroclinicity and relief (jebar) on large-s...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Described in this paper is a technique of using artificial water boundaries in theories of ocean cur...
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies...
The circulation in a coastal upwelling region with a shelf area is calculated. It is assumed that th...
The quasigeostrophic, wind-driven circulation theory given by Rhines and Young (1982b) is extended i...
Using the Monte Carlo method of statistical physics, we compute the equilibrium statistical mechanic...
The tides on a regular open coast change rapidly as a stonn approaches, and the time history of this...
The nature of the steady buoyancy-driven circulation is investigated using multi-level numerical mod...
The Large-scale Semi-Geostrophic Equations (LSGE, Salmon[73]) are three-dimensional equations valid ...
The assumption that surfaces of constant temperature and potential vorticity coincide leads to an ex...
A numerical exploration of inertial equilibrium states obtained with a primitive equation ocean mode...