Add to ORKGProfiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated form of the geostrophic relation
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Deep zonal jets in the western Pacific are geostrophic in character at latitudes of a fraction of a ...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
In the western North Pacific from 0-35N 130-180E, the vertical and horizontal thermal structure of t...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...