Forty freely drifting drogued buoys were tracked by satellite in the western tropical Pacific from June 1988 to January 1, 1990, as part of WEPOCS III. The data consist of buoy trajectories and sea surface temperature and velocity along trajectories. The main results presented here are the collection of figures which show trajectories and time series data in the South Equatorial Current, the North Equatorial Countercurrent, the Mindanao Current, and the North Equartorial Current. One striking result is that we obtained the first quasi-synoptic map of surface velocity in this region that shows the major currents and their interconnections.Funding was provided by the National Science Foundation through Grant No. OCE 87-16509
Hydrographic (0-1000 dbar) and direct current measurements (0-600 dbar) along 165-degrees-E (20-degr...
An analysis and interpretation of the position time series, and accompanying derived velocities, ob...
For centuries, our knowledge of the oceans ’ surface circulation was inferred from the drift of floa...
The Western Equatorial Pacific Ocean Circulation Study (WEPOCS) III expedition was conducted from Ju...
Tropical surface currents are estimated from satellite-derived surface topography and wind stress us...
Tropical surface currents are estimated from satellite-derived surface topography and wind stress us...
Thirty freely drifting drogued surface buoys were tracked by satellite in the vicinity of the Atlan...
A diagnostic model of the tropical circulation over the 0 ¡ 30m layer is derived by using quasi line...
Abstract. Tropical Pacific Ocean near-surface currents and their momentum and temperature balances a...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
Ship drift velocity observations were used to calculate and plot monthly mean and yearly mean veloc...
<p>(a) Averages for July–December 1997 (during a very intense El Niño) indicating the strong and ext...
Surface current measurements have been obtained from the Eastern tropical Pacific Ocean by means of ...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
Transport and thermohaline structure of water masses and their respective variability are observed a...
Hydrographic (0-1000 dbar) and direct current measurements (0-600 dbar) along 165-degrees-E (20-degr...
An analysis and interpretation of the position time series, and accompanying derived velocities, ob...
For centuries, our knowledge of the oceans ’ surface circulation was inferred from the drift of floa...
The Western Equatorial Pacific Ocean Circulation Study (WEPOCS) III expedition was conducted from Ju...
Tropical surface currents are estimated from satellite-derived surface topography and wind stress us...
Tropical surface currents are estimated from satellite-derived surface topography and wind stress us...
Thirty freely drifting drogued surface buoys were tracked by satellite in the vicinity of the Atlan...
A diagnostic model of the tropical circulation over the 0 ¡ 30m layer is derived by using quasi line...
Abstract. Tropical Pacific Ocean near-surface currents and their momentum and temperature balances a...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
Ship drift velocity observations were used to calculate and plot monthly mean and yearly mean veloc...
<p>(a) Averages for July–December 1997 (during a very intense El Niño) indicating the strong and ext...
Surface current measurements have been obtained from the Eastern tropical Pacific Ocean by means of ...
The upper and intermediate circulation (0-1200 m) in the western equatorial Pacific Ocean is examine...
Transport and thermohaline structure of water masses and their respective variability are observed a...
Hydrographic (0-1000 dbar) and direct current measurements (0-600 dbar) along 165-degrees-E (20-degr...
An analysis and interpretation of the position time series, and accompanying derived velocities, ob...
For centuries, our knowledge of the oceans ’ surface circulation was inferred from the drift of floa...