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Paleoceanography of the South China Sea and the western equatorial Pacific: Testing linkages between Indonesian Seaway closure and sea level change during the Middle to Late Miocene (～13--5 Ma)
Paleoceanography the equator the equator of the south China sea west Pacific sea level climate change
2014/10/22
The tectonic opening and closing of ocean gateways played a key role in global climate change during the Cenozoic. Although changes in these gateways affected ocean circulation and heat transport, man...
Variability in the Western Equatorial Pacific Ocean during the 1986–87 El Niño/Southern Oscillation Event
El Niñ o/Southern Oscillation Western Equatorial Pacific Ocean
2008/12/27
We describe variability in the western Pacific Ocean during the 1986–87 El Niño/Southern Oscillation (ENSO) event, with emphasis on time series measurements of currents, temperature, sea level ...
Surface Heat Fluxes in the Western Equatorial Pacific Ocean Estimated by Bulk Parameterization and by an Inverse Mixed Layer Model
Tropical Ocean Global Atmosphere Coupled Ocean–Atmosphere Response Experiment
2008/12/3
Sea surface heat fluxes in the western equatorial Pacific Ocean estimated by bulk parameterization are compared with fluxes computed with a one-dimensional, level 2.5 turbulence closure inverse mixed ...
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
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 ...
Modeling the Oceanic Response to Westerly Wind Bursts in the Western Equatorial Pacific
Western Equatorial Pacific Wind Bursts
2008/11/14
A 3D tropical upper-ocean circulation model is employed to study the generation mechanism for subsurface reversing currents forced by strong westerly wind bursts in the western equatorial Pacific. The...
Variations in Gyre Closure at the Water Mass Crossroads of the Western Equatorial Pacific Ocean
Variations Gyre Closure Water Mass Crossroads Western Equatorial Pacific Ocean
2008/7/25
Assuming the flow over the depth of interest may be described by a 2D streamfunction, , a general analytical method for determining the path of each streamline through a series of channels, which may ...
The Effect of Rainfall on the Surface Layer during a Westerly Wind Burst in the Western Equatorial Pacific
Surface Layer Westerly Wind Burst Western Equatorial Pacific
2008/7/10
Measurements of a fresh surface anomaly (fresh lens) produced by rainfall during a westerly wind burst have been analyzed. The measurements were made in December 1992 as part of the Coupled Ocean–Atmo...
Internal Solitary Waves in the Warm Pool of the Western Equatorial Pacific
Internal Solitary Waves Warm Pool Western Equatorial Pacific
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...
Impact of Sea Level Assimilation on Salinity Variability in the Western Equatorial Pacific
Sea Level Salinity Variability Western Equatorial Pacific
2008/7/1
In the primitive equation model for the tropical Pacific at the National Centers for Environmental Prediction, subsurface temperature observations are assimilated. The addition of TOPEX/Poseidon sea l...
Wind-Forced Reversing Jets in the Western Equatorial Pacific
Wind-Forced Reversing Jets Western Equatorial Pacific
2008/6/30
Upper-ocean zonal currents in the western equatorial Pacific are remarkably variable, changing direction both with time and depth. As a part of the Tropical Ocean and Global Atmosphere Coupled Ocean–A...
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
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...