Add to ORKGDirect measurements were made in 1980 and 1981 of the near-equatorial flow field along sections at 110, 102.5, 95, and 85W. The Equatorial Undercurrent weakens as it approaches the Galapagos. Most of the transport is lost from the warmer, upper part of the current...
Eddy momentum and heat fluxes are estimated from three-dimensional arrays of long time-series curren...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
project is about finding and describing a subsurface water current running parallel to and along the...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Eddy momentum and heat fluxes are estimated from three-dimensional arrays of long time-series curren...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E du...
A theoretical investigation is made of the wind as the possible cause of equatorial undercurrent. A ...
Two 100 km scale arrays of moored upper ocean current meters, one near 0, 152W, the other near 0, 11...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
Data from the Eastropac expedition in 1967–1968 and four subsequent cruises in 1970–1973 clearly ind...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
The Cromwell Current was observed in the eastern Pacific during the Scripps Institution of Oceanogra...
project is about finding and describing a subsurface water current running parallel to and along the...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
The presence of a southward-moving undercurrent along the west coast of South America, underlying th...
By mapping the distributions of the geostrophic flow and various water properties on the surface whe...
The low frequency fluctuations in the western Indian Ocean are dominated by energetic variability wi...
Eddy momentum and heat fluxes are estimated from three-dimensional arrays of long time-series curren...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
We develop a complete linear theory for the effects of islands on low frequency waves of the kind th...