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Closure of the Global Overturning Circulation Through the Indian, Pacific, and Southern Oceans: Schematics and Transports
Indian Pacific Southern Oceans
2015/7/16
The overturning pathways for the surface-ventilated North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW) and the diffusively formed Indian Deep Water (IDW) and Pacific Deep Water (PDW) a...
Effects of regional-scale and convective transports on tropospheric ozone chemistry revealed by aircraft observations during the wet season of the AMMA campaign
regional-scale and convective transports tropospheric ozone chemistry wet season
2009/3/12
The African Monsoon Multidisciplinary Analyses (AMMA) fourth airborne campaign was conducted in July–August 2006 to study the chemical composition of the middle and upper troposphere in West Africa wi...
Verification of Numerical Models of Lake Ontario III. Long-Term Heat Transports
Numerical Models Lake Ontario III Long-Term Heat Transports
2009/3/7
Numerical computations of water circulations, combined with observed temperature distribution, permit estimates of heat transports in Lake Ontario throughout the 1972 International Field Year. Weekly ...
Linking horizontal and vertical transports of biomass fire emissionsto the tropical Atlantic ozone paradox during the Northern Hemisphere winter season: climatology
biomass fire emissionsto tropical Atlantic ozone paradox Northern Hemisphere winter
2009/2/24
During the Northern hemisphere winter season, biomass burning is widespread in West Africa, yet the total tropospheric column ozone values (<30DU) over much of the Tropical Atlantic Ocean (15°N-5°S) ...
The Influence of Bottom Topography on Baroclinic Transports
Bottom Topography Baroclinic Transports
2009/2/6
A new and reduced set of governing equations is proposed for the modeling of baroclinic motions in a two-layer system with variable bottom topography. The reduction of the equations, which eliminates ...
Estimating the Meridional Energy Transports in the Atmosphere and Ocean
Meridional Energy Transports Atmosphere Ocean
2009/1/14
The poleward energy transports in the atmosphere–ocean system are estimated for the annual mean and the four seasons based on satellite measurements of the net radiation balance at the top of the atmo...
What is the fate of surface Ekman transport entering a subtropical gyre through its zonal boundaries? This question is investigated by resolving interior transport of a deep surface layer into nonvort...
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 ...
Dynamic Heights and Zonal Geostrophic Transports in the Central Tropical Pacific during 1979–84
temperature–salinity Dynamic Heights Zonal Geostrophic Transports Central Tropical Pacific
2009/1/6
Dynamic height is calculated from XBT and surface salinity data in the central Pacific using a mean temperature–salinity (T–S) relation in the usual way below the thermocline but assuming isohaline wa...
Ring Genesis and the Related Transports of Heat, Momentum and Vorticity：A Parameter Study
Ring Genesis Heat Momentum Vorticity
2008/12/30
The transport of heat, momentum and vorticity during the fife cycle of an unstable baroclinic wave that displays ring formation are investigated. Experiments have been carried out with a primitive equ...
Monthly Mean Wind Stress and Sverdrup Transports in the North Atlantic：A Comparison of the Hellerman–Rosenstein and Isemer–Hasse Climatologies
Isemer and Hasse Hellerman and Rosenstein Beaufort force
2008/12/23
The monthly mean wind stress climatology of Hellerman and Rosenstein (HR) is compared with the climatology of Isemer and Hasse (IH), which represents a version of the Bunker atlas (BU) for the North A...
A Description of COADS Surface Meteorological Fields and the Implied Sverdrup Transports for the Atlantic Ocean from 30°S to 60°N
Atlantic Ocean wind-driven circulation Sverdrup Transports Surface Meteorological Fields
2008/12/19
Using COADS data spanning 1947–1988, we describe the regional nature of the Atlantic Ocean wind-driven circulation between 30°8 and 60°N and its annual and interannual variability. The Sverdrup stream...
GEM/POPs: a global 3-D dynamic model for semi-volatile persistent organic pollutants – Part 2: Global transports and budgets of PCBs
3-D dynamic model semi-volatile persistent organic pollutants transports PCBs
2008/12/16
Global transports and budgets of three PCBs were investigated with a 3-D dynamic model for semi-volatile persistent organic pollutants – GEM/POPs. Dominant pathways were identified for PCB transports ...
The Formation of Oceanic Eddies in Symmetric and Asymmetric Jets. Part I：Early Time Evolution and Bulk Eddy Transports
Oceanic Eddies Symmetric Asymmetric Jets Bulk Eddy Transports
2008/12/12
A numerical study of the life cycles of eddies formed in perturbed baroclinic jets, emphasizing the influence of spanwise asymmetry in the initial structure of the jet on the downstream evolution of t...
Atmospheric Transports, the Thermohaline Circulation, and Flux Adjustments in a Simple Coupled Model
Atmospheric Transports Thermohaline Circulation Flux Adjustments Simple Coupled Model
2008/12/12
A theoretical analysis of the interactions between atmospheric meridional transports and the thermohaline circulation is presented, using a four-box ocean-atmosphere model in one hemisphere. The model...