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The Indonesian throughflow (ITF) is the flow of warm, relatively fresh waters into the southeast Indian Ocean from the western Pacific Ocean via the series of passages between the islands of the Indon...
A numerical model is used to mechanistically simulate the oceans seasonal cross-equatorial heat transport, and the results of Oort and Vonder Haar (1976). The basic process of Ekman pumping and drift...
Using hydrographic data of the IGY and METEOR expeditions, the inverse method of Wunsch (1978) has been applied to the subtropical South Atlantic Ocean to determine its general circulation and meridio...
The heat transported meridionally in the Pacific Ocean is calculated from the surface heat budgets of Clark and Weare and others; both budgets were based on Bunker's method with different radiation fo...
Estimates of oceanic meridional energy transport for the Pacific, Atlantic and Indian oceans are made using calculated annual mean surface energy fluxes. The surface flux calculations use bulk formula...
Estimates of oceanic meridional energy transport for the Pacific, Atlantic and Indian oceans are made using calculated annual mean surface energy fluxes. The surface flux calculations use bulk formula...
Direct velocity and temperature measurements obtained on a bimonthly basis from September 1980 to May 1983 in the Gulf Stream at 73°W longitude were used in combination with historical hydrographic an...
Various ocean circulation models have been compared with respect to their performance in the genesis of rings and the subsequent heat transport. Emphasis has been placed on the role of the spurious di...
The interannual heat budget of the Pacific equatorial upwelling zone is studied using a primitive equation, a reduced gravity model of the upper Pacific equatorial ocean. The model is forced with mont...
The seasonal heat transport mechanisms important in the Pacific equatorial upwelling zone are investigated using the primitive equation, reduced gravity model developed by Gent and Cane. Mechanisms of...
To avoid an explicit simulation of the overflows across the Greenland-Scotland ridge, many models of the large-scale ocean circulation seek to include the net effect of the inflowing dense water masse...
The role of mesoscale eddies in the poleward heat transport in the ocean is investigated; in particular, the compensation of poleward eddy heat transport by an eddy-induced mean meridional circulation...
Analyses of satellite-derived SSM/I winds and AVHRR sea surface temperatures are used to compute weekly estimates of global meridional ocean Ekman heat transport for the 4-year period 1987–1991. The h...
The author describes a series of mechanistic experiments showing the generation of interdecadal variability in the Bryan-Cox ocean general circulation model driven by a constant two-dimensional freshw...
Meridional heat transport in the North Pacific Ocean in a seasonally forced high-resolution global ocean general circulation model is compared to observations. At 24°N, annual mean heat transport ...

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