Add to ORKGFrom the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultaneously describe the wind stress, thermocline depth, surface current and transport of the Equatorial Undercurrent in the western equatorial Atlantic…
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
A study is conducted into the response of sea level and dynamic height to fluctuations of alongshore...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
A study is conducted into the response of sea level and dynamic height to fluctuations of alongshore...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Nonlinear solutions to the barotropic vorticity equation, forced by steady zonal winds and damped wi...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
This paper examines the response of the linear inviscid shallow water equations on a meridionally in...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...