CTD and velocity measurements were carried out in the western equatorial Pacific ocean at 165°E in april 1988. Large-scale structures along this meridian are first described. Then, preliminary results of an 8-day long station at the equator are used to locate layers of high variability. (Résumé d'auteur
As part of the verification phase of the TOPEX/POSEIDON mission, 10-day gridded fields of altimeter ...
The monitoring of upper ocean velocity, temperature, and surface winds at 0°, 170°W was initiated in...
The air-sea interaction thermodynamics of the western equatorial Pacific, the Earth\u27s largest reg...
In September 1988, the RRS Charles Darwin carried out a survey of the western equatorial Pacific bet...
Oceanographic observations using a CTD system were made in the Western Tropical Pacific in the summe...
A series of 12 meridional transect along longitude 165°E in the Western Equatorial Pacific ocean wer...
Twenty one oceanographic sections made along 165°E during 1984-1988 provide a unique picture of the ...
Oceanographic observations using a CTD system were made in the Western Tropical Pacific in the summe...
In support of the Tropical Ocean and Global Atmosphere (TOGA) program, investigators from the Woods ...
Turbulence measurements from the central equatorial Pacific in February 1982 have been analyzed and ...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
As part of the international TOGA program, the ORSTOM Center in Nouméa (New Caledonia) initiated in ...
In support of the Tropical Oceans and Global Atmosphere (TOGA) program, investigators from Woods Hol...
Oceanic current data in the warm pool region of the western equatorial Pacific measured by upward-lo...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
As part of the verification phase of the TOPEX/POSEIDON mission, 10-day gridded fields of altimeter ...
The monitoring of upper ocean velocity, temperature, and surface winds at 0°, 170°W was initiated in...
The air-sea interaction thermodynamics of the western equatorial Pacific, the Earth\u27s largest reg...
In September 1988, the RRS Charles Darwin carried out a survey of the western equatorial Pacific bet...
Oceanographic observations using a CTD system were made in the Western Tropical Pacific in the summe...
A series of 12 meridional transect along longitude 165°E in the Western Equatorial Pacific ocean wer...
Twenty one oceanographic sections made along 165°E during 1984-1988 provide a unique picture of the ...
Oceanographic observations using a CTD system were made in the Western Tropical Pacific in the summe...
In support of the Tropical Ocean and Global Atmosphere (TOGA) program, investigators from the Woods ...
Turbulence measurements from the central equatorial Pacific in February 1982 have been analyzed and ...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
As part of the international TOGA program, the ORSTOM Center in Nouméa (New Caledonia) initiated in ...
In support of the Tropical Oceans and Global Atmosphere (TOGA) program, investigators from Woods Hol...
Oceanic current data in the warm pool region of the western equatorial Pacific measured by upward-lo...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
As part of the verification phase of the TOPEX/POSEIDON mission, 10-day gridded fields of altimeter ...
The monitoring of upper ocean velocity, temperature, and surface winds at 0°, 170°W was initiated in...
The air-sea interaction thermodynamics of the western equatorial Pacific, the Earth\u27s largest reg...