Abstract: The results for two steady-state models of the world's ocean circulation are presented. The first model is of a homogeneous constant depth ocean with natural coastline geography. The second model, in addition, incorporates ...

Abstract: The transport in the western boundary layer in Stommel's model of the ocean circulation with a constant frictional coefficient over the entire basin is calculated exactly and is found to be significantly less than the ...

Abstract: A steady-state model of the ocean circulation applied to an ocean area surrounding New Zealand, driven by specified density and wind stress distributions and specified flow at the boundaries of the ocean area, has been ...

Abstract: When quasi-triennial periodicities have been found in climatic data, their presence has often been attributed to QBO-SO interaction. Although a mixture of idealized QBO and SO signals can give rise to a quasi-triennial ...