Add to ORKGThe total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reaches from the equator to about 50°S, and south of 40°S two cyclonic turns from the Circumpolar Current and Weddell Sea, west and east of the anticyclonic gyre. This figure has been changed very slightly between 40°S and 50°S from the figure shown in Reid (1994)..
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
Data from a hydrographic section carried out in January-March 1994 offshore from the eastern coast o...
The Verna Channel is a deep passage across the Rio Grande Rise in the South Atlantic through which A...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Mean total (barotropic + baroclinic) mass transports of the oceanic top 1000 dbar are estimated for ...
Zonal and meridional hydrographic sections obtained for the South Atlantic Ventilation Experiment ar...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
The Jungfem Passage Sill at a depth of 1815 meters is the controlling sill for the deepest water exc...
We use an inverse method to compute the deep circulation in the eastern South Pacific Ocean, on isop...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
Data from a hydrographic section carried out in January-March 1994 offshore from the eastern coast o...
The Verna Channel is a deep passage across the Rio Grande Rise in the South Atlantic through which A...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Mean total (barotropic + baroclinic) mass transports of the oceanic top 1000 dbar are estimated for ...
Zonal and meridional hydrographic sections obtained for the South Atlantic Ventilation Experiment ar...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
The Jungfem Passage Sill at a depth of 1815 meters is the controlling sill for the deepest water exc...
We use an inverse method to compute the deep circulation in the eastern South Pacific Ocean, on isop...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
A simplified three layer model is considered in order to examine the movements of deep mesoscale edd...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...