Add to ORKGAn isolated barotropic eddy on the β-plane can be in equilibrium only if it is composed of a coupled cyclone-anticyclone system, only if it is separated by a vorticity discontinuity (free streamline) from the surrounding fluid..
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
The problem of forced, geostrophic turbulence in a basin is revisited. The primary focus is the time...
It is well known that the barotropic, wind-driven, single-gyre ocean model reaches an inertially-dom...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
Results from several numerical experiments based on one class of eddy-resolving gyre-scale models ha...
Using boundary-enhanced viscosity to control the mean circulation, a simple model can be created and...
The quasigeostrophic, wind-driven circulation theory given by Rhines and Young (1982b) is extended i...
A deterministic model is developed to evaluate and explain the rate of dissipation of momentum in ed...
Thesis (Ph.D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept....
A barotropic model is employed to study the dynamics of colliding jets along a western boundary. To ...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
A series of multi-layer numerical experiments show that classical finite amplitude instabilities in ...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
The problem of forced, geostrophic turbulence in a basin is revisited. The primary focus is the time...
It is well known that the barotropic, wind-driven, single-gyre ocean model reaches an inertially-dom...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
Results from several numerical experiments based on one class of eddy-resolving gyre-scale models ha...
Using boundary-enhanced viscosity to control the mean circulation, a simple model can be created and...
The quasigeostrophic, wind-driven circulation theory given by Rhines and Young (1982b) is extended i...
A deterministic model is developed to evaluate and explain the rate of dissipation of momentum in ed...
Thesis (Ph.D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept....
A barotropic model is employed to study the dynamics of colliding jets along a western boundary. To ...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
A series of multi-layer numerical experiments show that classical finite amplitude instabilities in ...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
A class of exact solutions of the equation of conservation of the quasi-geostrophic vorticity in a c...
The problem of forced, geostrophic turbulence in a basin is revisited. The primary focus is the time...