Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 110W, were used to study the zonal transport of the strong equatorial currents in and above the thermocline. At long periods (several days), fluctuations· in the vertically integrated zonal velocity (transport per unit meridional distance) at a single equatorial mooring were highly correlated with fluctuations in the total transport across the section 0-250 m and 1N-1S, which includes most of the Equatorial Undercurrent...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
A linear theory is presented for the flow of equatorial Kelvin waves and of the equatorial undercurr...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Eddy momentum and heat fluxes are estimated from three-dimensional arrays of long time-series curren...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Eart...
This paper uses a theoretical model to demonstrate the existence of a group of equatorially trapped,...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
A linear theory is presented for the flow of equatorial Kelvin waves and of the equatorial undercurr...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Eddy momentum and heat fluxes are estimated from three-dimensional arrays of long time-series curren...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Thesis (Ph. D.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Eart...
This paper uses a theoretical model to demonstrate the existence of a group of equatorially trapped,...
The problem of an equatorial Kelvin wave of step-function form incident on an eastern meridional bou...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...