Add to ORKGThe quasigeostrophic, wind-driven circulation theory given by Rhines and Young (1982b) is extended in two directions. First, we consider forcing patterns which are not contrived so as to close without a western boundary layer. The resulting barotropic circulation pattern (see Fig. 1) has the well known east-west asymmetry produced by the β-effect...
Using a two-layer quasigeostrophic model with weak interfacial and bottom friction we propose a mech...
Author Posting. © Sears Foundation for Marine Research, 2004. This article is posted here by permis...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
It is well known that the barotropic, wind-driven, single-gyre ocean model reaches an inertially-dom...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Using boundary-enhanced viscosity to control the mean circulation, a simple model can be created and...
We investigate the steady barotropic circulation patterns driven by inflow-outflow boundary conditio...
This work examines the instabilities of steady circulations driven by stationary single-gyre wind fo...
The steady large scale oceanic response to wind stress and a surface buoyancy flux is studied by mak...
Baroclinic flow over a western continental slope is investigated using a simple model in which inert...
Multiple equilibria of the wind-driven gyres have been found in idealized quasi-geostrophic and shal...
Within a quasi-geostrophic two-layer model of the wind-driven ocean circulation, an idealized symmet...
A barotropic model of the wind-driven circulation in the subtropical region of the ocean is consider...
Using a two-layer quasigeostrophic model with weak interfacial and bottom friction we propose a mech...
Author Posting. © Sears Foundation for Marine Research, 2004. This article is posted here by permis...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
It is well known that the barotropic, wind-driven, single-gyre ocean model reaches an inertially-dom...
An analytical model is developed for the wind-driven circulation in a continuously stratified ocean ...
Using boundary-enhanced viscosity to control the mean circulation, a simple model can be created and...
We investigate the steady barotropic circulation patterns driven by inflow-outflow boundary conditio...
This work examines the instabilities of steady circulations driven by stationary single-gyre wind fo...
The steady large scale oceanic response to wind stress and a surface buoyancy flux is studied by mak...
Baroclinic flow over a western continental slope is investigated using a simple model in which inert...
Multiple equilibria of the wind-driven gyres have been found in idealized quasi-geostrophic and shal...
Within a quasi-geostrophic two-layer model of the wind-driven ocean circulation, an idealized symmet...
A barotropic model of the wind-driven circulation in the subtropical region of the ocean is consider...
Using a two-layer quasigeostrophic model with weak interfacial and bottom friction we propose a mech...
Author Posting. © Sears Foundation for Marine Research, 2004. This article is posted here by permis...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...