Add to ORKGThe presence of a southward-moving undercurrent along the west coast of South America, underlying the Peru Current at depths of several hundred meters, has been established by direct measurements with parachute drogues, by calculations of geostrophic motion, and by analysis of the distributions of salinity and dissolved oxygen...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
During November-December 1977, a modest physical field experiment was carried out over the wide shel...
In December, 1975, an upwelling study was conducted at Punta Curaumilla near Valparaiso, Chile. Prev...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
Profiles of chlorophyll a, temperature and salinity were measured over the Peru Shelf at 9S. Data we...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
It has generally been considered that the Guiana Current carries South Atlantic Central water in an ...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
During November-December 1977, a modest physical field experiment was carried out over the wide shel...
In December, 1975, an upwelling study was conducted at Punta Curaumilla near Valparaiso, Chile. Prev...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
Profiles of chlorophyll a, temperature and salinity were measured over the Peru Shelf at 9S. Data we...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...