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PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES
Nutrients Phosphorus Cycle Glacial-Interglacial Sea Level
2015/1/16
Paleoproductivity records during the late Pleistocene are sparse. The equatorial Pacific and the Southern Ocean are collectively responsible for the majority of the new production in the oceans. The n...
Wind-Forced Variability of Upper Ocean Dynamics in the Central Equatorial Pacific during PEQUOD
Wind-Forced Variability Central Equatorial Pacific Upper Ocean Dynamics
2009/1/19
Horizontal currants and dynamic height anomalies measured with a vertical profiler in the central equatorial Pacific during January 1981, February 1982 and April 1982 show significant changes in the u...
The Annual Rossby Wave in the Central Equatorial Pacific Ocean
Annual Rossby Wave Central Equatorial Pacific Ocean
2009/1/14
We attribute observed annual variations in the subthermocline thermal structure of the central equatorial Pacific to a forced gravest-meridional-mode Rossby wave. In the region between 300 and 800 m (...
Mixed-Layer Shear Generated by Wind Stress in the Central Equatorial Pacific
Mixed-Layer Shear Central Equatorial Pacific Wind Stress
2008/12/30
Sixteen months of wind and current profile observations in the central equatorial Pacific show the response of the upper-ocean shear to local wind forcing. The shear at the ocean surface is significan...
Vertical Structure of the Seasonal Cycle in the Central Equatorial Atlantic Ocean：XBT Sections from 1980 to 1988
Vertical Structure Central Equatorial Atlantic Ocean Seasonal Cycle
2008/12/23
A set of temperature profiles from expendable bathythermographs collected from 1980 to April 1988 along two ship routes transecting the equatorial Atlantic from 11°N to 11°S is analyzed to inter the v...
Why Is There a Tritium Maximum in the Central Equatorial Pacific Thermocline?
Central Equatorial North Equatorial Countercurrent
2008/10/27
It is suggested that the tritium maximum in the central Pacific is caused by two water pathways across the North Equatorial Countercurrent (NECC), one from the central Pacific and the other from the M...
Internal Waves and Turbulence in the Upper Central Equatorial Pacific: Lagrangian and Eulerian Observations
Internal Waves Turbulence Upper Central Equatorial Pacific Eulerian Observations
2008/6/13
In the shear stratified flow below the surface mixed layer in the central equatorial Pacific, energetic near-N (buoyancy frequency) internal waves and turbulence mixing were observed by the combinatio...