Add to ORKGThe Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanography SWAN SONG Expedition, 5 September–1 December 1961, employing hydrographic stations and direct current measurements. The velocity structure in 1961 at 140°W was similar to that observed in April 1958 except that the transport in 1961 was only 22 × 106 m3 /sec---55% of the transport observed in 1958...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
An array of near-bottom current meters was set on the continental rise and slope near Site D in the ...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
A bathythermograph section generated during the outward run along a roo mile line running 255° from ...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
During June 1966, nine velocity measurements were made with neutrally buoyant floats at a depth of a...
This paper contains selected results from the first in a series of new efforts directed toward estab...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
An array of near-bottom current meters was set on the continental rise and slope near Site D in the ...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Direct measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 1...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
A bathythermograph section generated during the outward run along a roo mile line running 255° from ...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
During June 1966, nine velocity measurements were made with neutrally buoyant floats at a depth of a...
This paper contains selected results from the first in a series of new efforts directed toward estab...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
An array of near-bottom current meters was set on the continental rise and slope near Site D in the ...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...