Add to ORKGAll available navifacial data from 1956 to 1974 have been compiled to produce two charts per year of surface salinity between 150°E and 130°W and between 10°N and 25°S. On each chart, the following m ain features are observed: south of 10°S and east of 160°W the tropical salinity maximum extending westward south of the equator; and a salinity minimum from 5°S to 20°S and west of 170°W. The oscillations of the position and intensity of these features are not all seasonal...
Climate observations in much of the tropical oceans are scarce during most of the 20th century, so p...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Sea Surface Salinity (SSS) data have been collected in the Tropical Pacific Ocean since 1969. From t...
Sea surface bucket measurements, obtained through a ship-of-opportunity program, are used to describ...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The dominant mode of variability in the tropical Pacific is the interannual El Nino-Southern Oscilla...
Seasonal variations in sea level derived from IGY measurements are described and compared with those...
This paper finds a north‐south contrast of subsurface salinity trend during 2002–2013 in the northwe...
Climate observations in much of the tropical oceans are scarce during most of the 20th century, so p...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Between 24 July and 10 September 1964, low sea-surface salinity was present off South America betwee...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Sea Surface Salinity (SSS) data have been collected in the Tropical Pacific Ocean since 1969. From t...
Sea surface bucket measurements, obtained through a ship-of-opportunity program, are used to describ...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The dominant mode of variability in the tropical Pacific is the interannual El Nino-Southern Oscilla...
Seasonal variations in sea level derived from IGY measurements are described and compared with those...
This paper finds a north‐south contrast of subsurface salinity trend during 2002–2013 in the northwe...
Climate observations in much of the tropical oceans are scarce during most of the 20th century, so p...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...