Add to ORKGBetween 24 July and 10 September 1964, low sea-surface salinity was present off South America between 5°N and 100°N in the form of two partly merged tongues extending more than 600 n. mi. east of 50°W. Near 9°N, 50°W, a marked eastward flow was found and identified as the Equatorial Counter Current; it apparently brought in much of the freshened water encountered east of 50°W...
The influence of the Amazon River discharge on the nutrient chemistry and biological productivity in...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Surface temperature and salinity maps from measurements during the period of maximum coastal upwelli...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
All available navifacial data from 1956 to 1974 have been compiled to produce two charts per year of...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The seasonal surface salinity regime near Barbados, West Indies is explained in terms of the oceanog...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
During November-December 1977, a modest physical field experiment was carried out over the wide shel...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
During the summer of 1955, record high sea water temperatures were observed in harbors and coastal w...
The influence of the Amazon River discharge on the nutrient chemistry and biological productivity in...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Surface temperature and salinity maps from measurements during the period of maximum coastal upwelli...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
All available navifacial data from 1956 to 1974 have been compiled to produce two charts per year of...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The seasonal surface salinity regime near Barbados, West Indies is explained in terms of the oceanog...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
During November-December 1977, a modest physical field experiment was carried out over the wide shel...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
During the summer of 1955, record high sea water temperatures were observed in harbors and coastal w...
The influence of the Amazon River discharge on the nutrient chemistry and biological productivity in...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Surface temperature and salinity maps from measurements during the period of maximum coastal upwelli...