Add to ORKGA method is developed for calculating the response of an unbounded inviscid ocean to wind stress and thermal forcings. Although emphasis is on equatorial baroclinic motions, the mathematical technique is first illustrated in detail for the motions described by the similar but simpler barotropic vorticity equation. This serves to clarify the significance of the asymptotic approximations made for the baroclinic planetary modes...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...
The strength of the East Australian Current (EAC) is observed to vary in response to changes in basi...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
Standing equatorial wave modes are shown to be exact solutions of the forced, linear, inviscid shall...
The effect of upper ocean variability on deep equatorial flow is simulated by prescribing a forcing ...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
A noneddy resolving, time-dependent, nonlinear theory of the large-scale ocean circulation is presen...
This paper concerns the linear response of the ocean to forcing at a specified frequency and wave nu...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Investigation is made into the response of an equatorial ocean to growing and moving zonal wind syst...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...
The strength of the East Australian Current (EAC) is observed to vary in response to changes in basi...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
Standing equatorial wave modes are shown to be exact solutions of the forced, linear, inviscid shall...
The effect of upper ocean variability on deep equatorial flow is simulated by prescribing a forcing ...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
A noneddy resolving, time-dependent, nonlinear theory of the large-scale ocean circulation is presen...
This paper concerns the linear response of the ocean to forcing at a specified frequency and wave nu...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Investigation is made into the response of an equatorial ocean to growing and moving zonal wind syst...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A linear primitive equations model is used to simulate spin-up of a two-layer ocean bisected by a me...
The strength of the East Australian Current (EAC) is observed to vary in response to changes in basi...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...