Add to ORKGBasin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlantic between 32 and 53N. The absolute velocity on each section has been chosen so that the transport satisfies the Sverdrup relation. It is concluded that the wind-driven currents are not confined to the upper thermocline but extend to great depth...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
We estimate the time-averaged velocity field in the North Atlantic from observations of density, win...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
A comparison is made between the geostrophic transport across selected latitudes in the North Atlant...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
In order to produce a long-term mean circulation pattern for the western North Atlantic, geostrophic...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The first long-term (250 d) current measurements from the southern trough of the CharlieGibbs Fractu...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
We estimate the time-averaged velocity field in the North Atlantic from observations of density, win...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
A comparison is made between the geostrophic transport across selected latitudes in the North Atlant...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
In order to produce a long-term mean circulation pattern for the western North Atlantic, geostrophic...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The first long-term (250 d) current measurements from the southern trough of the CharlieGibbs Fractu...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
We estimate the time-averaged velocity field in the North Atlantic from observations of density, win...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...