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Advective transport of diazotrophs and importance of their nitrogen fixation on new and primary production in the western Pacific warm pool
Advective transport diazotrophs importance their nitrogen fixation new primary production in the western Pacific warm pool
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2014/4/2
The western Pacific warm pool (WPWP) is a region of low nutrient and chlorophyll concentrations in which new production is generally considered to be supported by upward fluxes of nitrate from the dee...
Lagrangian drifter paths and length scales in the tropical Pacific warm pool from 1990 to 1991:with application of fractal techniques
Lagrangian drifter paths length scales tropical Pacific warm pool fractal techniques
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2009/11/16
This paper presents an analysis of WOCE/TOGA surface drifter paths and its interpretation in conjunction with the west Pacific warm pool water motion. Our interest here lies in the existence of scale ...
Sharp Frontal Interfaces in the Near-Surface Layer of the Ocean in the Western Equatorial Pacific Warm Pool
surface layer western Pacific warm pool horizontal temperature salinity variability
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2008/11/18
During the TOGA COARE rich horizontal temperature and salinity variability of the near-surface layer of the ocean in the western Pacific warm pool was observed. High-resolution measurements were made ...
Centroid Motion of the Western Pacific Warm Pool during Three Recent El Niño–Southern Oscillation Events
Centroid Motion El Niñ o–Southern Oscillation Events Western Pacific Warm Pool
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2008/11/18
The centroid motion of the Western Pacific warm pool for 1982–83, 1986–87 and 1991–93 El Niño–Southern Oscillation events was investigated by analyzing satellite multichannel sea surface temper...
Internal Solitary Waves in the Warm Pool of the Western Equatorial Pacific
Internal Solitary Waves Warm Pool Western Equatorial Pacific
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2008/7/3
During the spring tides of late November 1992, early January and early February 1993, solitary internal wave packets were observed at 2°S, 156°15′E in the western equatorial Pacific. Apparently genera...
A Simple Warm-Pool Displacement ENSO Model
Simple Warm-Pool ENSO Model
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2008/7/1
The authors derive analytical and numerical solutions to a simple model of the zonal displacement of the western equatorial Pacific warm pool. The model is based on a single variable x(t), the anomalo...
Horizontal Structure of the Upper Ocean Velocity and Density Fields in the Western Equatorial Pacific Warm Pool: Depth Range from 20 to 250 m
Horizontal Structure Upper Ocean Velocity Density Fields Western Equatorial Pacific
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2008/6/30
Wavenumber spectra of velocity and density fields in the western equatorial Pacific warm pool on scales 6–120 km are estimated using the shipboard survey data collected during the TOGA Coupled Ocean–A...