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Upper Ocean Water Masses and Transports in the Western Tropical Pacific (165°E)
Equatorial Undercurrent South Equatorial Current South Subsurface Countercurrents
2009/1/9
As part of the international TOGA program, the ORSTOM Center in Nouméa (New Caledonia) initiated in January 1984 a series of semi-annual cruises along the 165°E meridian from 20°S to 10°N, across the ...
The Water Masses of the Central North Atlantic in 1983—84
Water Masses Central North Atlantic
2009/1/6
Hydrographic surveys carried out in 1983–84 along both sides of the Mid-Atlantic Ridge between 24° and 53°N provide a detailed description of the well-known North Atlantic water masses with particular...
Currents, Water Masses, Eddies and Jets in the Mediterranean Levantine Basin
Atlantic Water Levantine Surface Water Levantine Intermediate Waters empirical orthogonal function
2009/1/6
Hydrographic measurements in the southeastern Levantine basin are analyzed, and the climatological water masses of the region and their seasonal variations are identified. We observe the formation of ...
An Idealized Model of the World Ocean. Part I：The Global-Scale Water Masses
Idealized Model World Ocean Global-Scale Water Masses
2009/1/5
A primitive equation, three-dimensional numerical model of the ocean, employing idealized versions of the real topography and surface boundary conditions, is used to study the water mass structure of ...
Representing the Global-Scale Water Masses in Ocean General Circulation Models
North Atlantic Deep Wate Antarctic Intermediate Water Global-Scale Water Masses
2008/12/18
A hierarchy of coarse-resolution World Ocean experiments were integrated with a view to determining the most appropriate representation of the global-scale water masses in ocean general circulation mo...
Global-Scale Water Masses, Meridional Circulation, and Heat Transport Simulated with a Global Isopycnal Ocean Model
Global-Scale Water Masses Meridional Circulation Heat Transport isopycnal ocean models
2008/11/11
The goal of this study is to fill the gap in equilibrium solutions of the global-scale water masses, meridional circulation, and heat transport with isopycnal ocean models. To this end, a global isopy...
Influences of Topography on the Modeling of Abyssal Water Masses. Part I: Effects of Channel Representation
Topography Modeling of Abyssal Water Masses Channel Representation
2008/7/23
Connections between basins below 4000 m, which may or may not be resolved in computer-generated model topography, have been found to have a considerable impact on the movement of Antarctic Bottom Wate...
Influences of Topography on the Modeling of Abyssal Water Masses. Part II: Spurious Extrema
Topography Abyssal Water Masses Spurious Extrema
2008/7/23
Unphysical extrema are found in ocean simulations employing space-centered advection even when horizontal mixing coefficients are sufficient to suppress checkerboard behavior. They are mostly found as...